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SOE.bib
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@article{mills_fisheries_2013,
title = {Fisheries Management in a Changing Climate: Lessons From the 2012 Ocean Heat Wave in the Northwest Atlantic},
volume = {26},
issn = {10428275},
url = {https://tos.org/oceanography/article/fisheries-management-in-a-changing-climate-lessonsfrom-the-2012-ocean-heat-},
doi = {10.5670/oceanog.2013.27},
shorttitle = {Fisheries Management in a Changing Climate},
number = {2},
journaltitle = {Oceanography},
shortjournal = {oceanog},
author = {Mills, Katherine and Pershing, Andrew and Brown, Curtis and Chen, Yong and Chiang, Fu-Sung and Holland, Daniel and Lehuta, Sigrid and Nye, Janet and Sun, Jenny and Thomas, Andrew and Wahle, Richard},
urldate = {2020-02-10},
date = {2013},
file = {Full Text:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\DY4W3JYE\\Mills et al. - 2013 - Fisheries Management in a Changing Climate Lesson.pdf:application/pdf},
}
@article{lawson_important_1998,
title = {Important prey species of marine vertebrate predators in the northwest Atlantic: proximate composition and energy density},
volume = {164},
issn = {0171-8630},
url = {https://www.jstor.org/stable/24825521},
shorttitle = {Important prey species of marine vertebrate predators in the northwest Atlantic},
abstract = {Prey energy density values are crucial inputs to bioenergetic consumption models. Vertebrate predators in the northwest Atlantic consume a variety of prey species, but the proximate composition ({PC}; proportions of lipid, protein, ash and water) and energy density ({ED}; {kJ} g–1) of prey, and their variability, are known poorly. In this study, key prey species from Newfoundland and Labrador were studied: Atlantic cod Gadus morhua, American plaice Hippoglossoides platessoides, sand lance Ammodytes dubius, Arctic cod Boreogadus saida, northern shrimp Pandalus borealis, redfish Sebastes spp., Greenland halibut Reinhardtius hippoglossoides, squid Illex illecebrosus and Gonatus fabricii, capelin Mallotus villosus, Atlantic herring Clupea harengus and daubed shanny Lumpenus maculatus. {PC} and {ED} varied greatly among species and were influenced by size, season, geography and year. Herring, capelin and G. fabricii had the highest {ED}, whereas Atlantic cod, plaice, sand lance and shrimp had the lowest. Halibut and I. illecebrosus increased in {ED} with size. {EDs} of capelin and redfish varied seasonally; that of plaice and sand lance did not. Herring and halibut had higher {ED} in the early 1990s than in recent years. Such variation in prey {ED} has important implications for digestive efficiency, foraging energetics, and dietary preferences of vertebrate predators.},
pages = {13--20},
journaltitle = {Marine Ecology Progress Series},
author = {Lawson, John W. and Magalhães, Alexandra M. and Miller, Edward H.},
urldate = {2020-02-13},
date = {1998},
}
@article{hobday_hierarchical_2016,
title = {A hierarchical approach to defining marine heatwaves},
volume = {141},
issn = {0079-6611},
url = {http://www.sciencedirect.com/science/article/pii/S0079661116000057},
doi = {10.1016/j.pocean.2015.12.014},
abstract = {Marine heatwaves ({MHWs}) have been observed around the world and are expected to increase in intensity and frequency under anthropogenic climate change. A variety of impacts have been associated with these anomalous events, including shifts in species ranges, local extinctions and economic impacts on seafood industries through declines in important fishery species and impacts on aquaculture. Extreme temperatures are increasingly seen as important influences on biological systems, yet a consistent definition of {MHWs} does not exist. A clear definition will facilitate retrospective comparisons between {MHWs}, enabling the synthesis and a mechanistic understanding of the role of {MHWs} in marine ecosystems. Building on research into atmospheric heatwaves, we propose both a general and specific definition for {MHWs}, based on a hierarchy of metrics that allow for different data sets to be used in identifying {MHWs}. We generally define a {MHW} as a prolonged discrete anomalously warm water event that can be described by its duration, intensity, rate of evolution, and spatial extent. Specifically, we consider an anomalously warm event to be a {MHW} if it lasts for five or more days, with temperatures warmer than the 90th percentile based on a 30-year historical baseline period. This structure provides flexibility with regard to the description of {MHWs} and transparency in communicating {MHWs} to a general audience. The use of these metrics is illustrated for three 21st century {MHWs}; the northern Mediterranean event in 2003, the Western Australia ‘Ningaloo Niño’ in 2011, and the northwest Atlantic event in 2012. We recommend a specific quantitative definition for {MHWs} to facilitate global comparisons and to advance our understanding of these phenomena.},
pages = {227--238},
journaltitle = {Progress in Oceanography},
shortjournal = {Progress in Oceanography},
author = {Hobday, Alistair J. and Alexander, Lisa V. and Perkins, Sarah E. and Smale, Dan A. and Straub, Sandra C. and Oliver, Eric C. J. and Benthuysen, Jessica A. and Burrows, Michael T. and Donat, Markus G. and Feng, Ming and Holbrook, Neil J. and Moore, Pippa J. and Scannell, Hillary A. and Sen Gupta, Alex and Wernberg, Thomas},
urldate = {2020-02-10},
date = {2016-02-01},
langid = {english},
file = {ScienceDirect Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\EAJ6P3XR\\Hobday et al. - 2016 - A hierarchical approach to defining marine heatwav.pdf:application/pdf;ScienceDirect Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\B4WY7WYM\\S0079661116000057.html:text/html},
}
@article{steimle_energy_1985,
title = {Energy Equivalents of Marine Organisms from the Continental Shelf of the Temperate Northwest Atlantic},
volume = {6},
doi = {10.2960/J.v6.a11},
abstract = {The availability of appropriate energy equivalents is one of the needs in species or community bioenergetic models. Energy equivalent data for 151 common invertebrate and vertebrate species on the continental shelf of the temperate Northwest Atlantic from Nova Scotia to North Carolina are presented and compared with the more limited results of other studies. Energy equivalents were found to be variable among major taxonomic ortrophic groups and general trends were not evident. A review of equivalents from some recent ecosystem models for the Northwest Atlnatic indicates that the models can be substantially improved.},
journaltitle = {Journal of Northwest Atlantic Fishery Science},
shortjournal = {Journal of Northwest Atlantic Fishery Science},
author = {Steimle, Frank and Terranova, Russell},
date = {1985-12-01},
file = {Full Text:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\C3HQBRTS\\Jr and Terranova - 1985 - Energy Equivalents of Marine Organisms from the Co.pdf:application/pdf},
}
@article{tam_comparing_2017,
title = {Comparing Apples to Oranges: Common Trends and Thresholds in Anthropogenic and Environmental Pressures across Multiple Marine Ecosystems},
volume = {4},
issn = {2296-7745},
url = {https://www.frontiersin.org/articles/10.3389/fmars.2017.00282/full},
doi = {10.3389/fmars.2017.00282},
shorttitle = {Comparing Apples to Oranges},
abstract = {Ecosystem-based management ({EBM}) in marine ecosystems considers impacts caused by complex interactions between environmental and anthropogenic pressures (i.e. oceanographic, climatic, socio-economic) and marine communities. {EBM} depends, in part, on ecological indicators that facilitate understanding of inherent properties and the dynamics of pressures within marine communities. Thresholds of ecological indicators delineate ecosystem status because they represent points at which a small increase in one or many pressure variables results in an abrupt change of ecosystem responses. The difficulty in developing appropriate thresholds and reference points for {EBM} lies in the multidimensionality of both the ecosystem responses and the pressures impacting the ecosystem. Here, we develop thresholds using gradient forest for a suite of ecological indicators in response to multiple pressures that convey ecosystem status for large marine ecosystems from the {US} Pacific, Atlantic, sub-Arctic, and Gulf of Mexico. We detected these thresholds of ecological indicators based on multiple pressures. Commercial fisheries landings above approximately 2-4.5 t km-2 and fisheries exploitation above 20-40\% of the total estimated biomass (of invertebrates and fish) of the ecosystem resulted in a change in the direction of ecosystem structure and functioning in the ecosystems examined. Our comparative findings reveal common trends in ecosystem thresholds along pressure gradients and also indicate that thresholds of ecological indicators are useful tools for comparing the impacts of environmental and anthropogenic pressures across multiple ecosystems. These critical points can be used to inform the development of {EBM} decision criteria.},
journaltitle = {Frontiers in Marine Science},
shortjournal = {Front. Mar. Sci.},
author = {Tam, Jamie C. and Link, Jason S. and Large, Scott I. and Andrews, Kelly and Friedland, Kevin D. and Gove, Jamison and Hazen, Elliott and Holsman, Kirstin and Karnauskas, Mandy and Samhouri, Jameal F. and Shuford, Rebecca and Tomilieri, Nick and Zador, Stephani},
urldate = {2020-03-09},
date = {2017},
note = {Publisher: Frontiers},
keywords = {anthropogenic and environmental pressures, comparative analysis, Ecological Indicators, ecosystem-based management, Gradient forest, thresholds-based reference points},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\RTFYBX68\\Tam et al. - 2017 - Comparing Apples to Oranges Common Trends and Thr.pdf:application/pdf},
}
@article{thorson_guidance_2019,
title = {Guidance for decisions using the Vector Autoregressive Spatio-Temporal ({VAST}) package in stock, ecosystem, habitat and climate assessments},
volume = {210},
issn = {0165-7836},
url = {http://www.sciencedirect.com/science/article/pii/S0165783618302820},
doi = {10.1016/j.fishres.2018.10.013},
abstract = {Fisheries scientists provide stock, ecosystem, habitat, and climate assessments to support interdisplinary fisheries management in the {US} and worldwide. These assessment activities have evolved different models, using different review standards, and are communicated using different vocabulary. Recent research shows that spatio-temporal models can estimate population density for multiple locations, times, and species, and that this is a “common currency” for addressing core goals in stock, ecosystem, habitat, and climate assessments. I therefore review the history and “design principles” for one spatio-temporal modelling package, the Vector Autoregressive Spatio-Temporal ({VAST}) package. I then provide guidance on fifteen major decisions that must be made by users of {VAST}, including: whether to use a univariate or multivariate model; when to include spatial and/or spatio-temporal variation; how many factors to use within a multivariate model; whether to include density or catchability covariates; and when to include a temporal correlation on model components. I finally demonstrate these decisions using three case studies. The first develops indices of abundance, distribution shift, and range expansion for arrowtooth flounder (Atheresthes stomias) in the Eastern Bering Sea, showing the range expansion for this species. The second involves “species ordination” of eight groundfishes in the Gulf of Alaska bottom trawl survey, which highlights the different spatial distribution of flathead sole (Hippoglossoides elassodon) relative to sablefish (Anoplopoma fimbria) and dover sole (Microstomus pacificus). The third involves a short-term forecast of the proportion of coastwide abundance for five groundfishes within three spatial strata in the {US} West Coast groundfish bottom trawl survey, and predicts large interannual variability (and high uncertainty) in the distribution of lingcod (Ophiodon elongatus). I conclude by recommending further research exploring the benefits and limitations of a “common currency” approach to stock, ecosystem, habitat, and climate assessments, and discuss extending this approach to optimal survey design and economic assessments.},
pages = {143--161},
journaltitle = {Fisheries Research},
shortjournal = {Fisheries Research},
author = {Thorson, James T.},
urldate = {2020-02-24},
date = {2019-02-01},
langid = {english},
keywords = {Climate vulnerability analysis, Distribution shift, Habitat assessment, Index standardization, Integrated ecosystem assessment, Spatio-temporal model, Stock assessment, {VAST}},
file = {ScienceDirect Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\W7IBXWVK\\Thorson - 2019 - Guidance for decisions using the Vector Autoregres.pdf:application/pdf;ScienceDirect Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\V3KPTUYK\\S0165783618302820.html:text/html},
}
@article{hardison_simulation_2019,
title = {A simulation study of trend detection methods for integrated ecosystem assessment},
volume = {76},
issn = {1054-3139},
url = {https://academic.oup.com/icesjms/article/76/7/2060/5512306},
doi = {10.1093/icesjms/fsz097},
abstract = {Abstract. The identification of trends in ecosystem indicators has become a core component of ecosystem approaches to resource management, although oftentimes},
pages = {2060--2069},
number = {7},
journaltitle = {{ICES} Journal of Marine Science},
shortjournal = {{ICES} J Mar Sci},
author = {Hardison, Sean and Perretti, Charles T. and {DePiper}, Geret S. and Beet, Andrew},
urldate = {2020-02-26},
date = {2019-12-01},
langid = {english},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\TCF5T9KA\\Hardison et al. - 2019 - A simulation study of trend detection methods for .pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\77FEQEX7\\5512306.html:text/html},
}
@article{ekstrom_vulnerability_2015,
title = {Vulnerability and adaptation of {US} shellfisheries to ocean acidification},
volume = {5},
rights = {2015 Nature Publishing Group, a division of Macmillan Publishers Limited. All Rights Reserved.},
issn = {1758-6798},
url = {https://www.nature.com/articles/nclimate2508},
doi = {10.1038/nclimate2508},
abstract = {Understanding the vulnerability of different {US} coastal communities to the likely harmful effects of ocean acidification on shellfisheries should inform the development of effective adaptation measures.},
pages = {207--214},
number = {3},
journaltitle = {Nature Climate Change},
author = {Ekstrom, Julia A. and Suatoni, Lisa and Cooley, Sarah R. and Pendleton, Linwood H. and Waldbusser, George G. and Cinner, Josh E. and Ritter, Jessica and Langdon, Chris and van Hooidonk, Ruben and Gledhill, Dwight and Wellman, Katharine and Beck, Michael W. and Brander, Luke M. and Rittschof, Dan and Doherty, Carolyn and Edwards, Peter E. T. and Portela, Rosimeiry},
urldate = {2020-03-06},
date = {2015-03},
langid = {english},
note = {Number: 3
Publisher: Nature Publishing Group},
file = {Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\XJCI7DCX\\nclimate2508.html:text/html},
}
@article{large_defining_2013,
title = {Defining trends and thresholds in responses of ecological indicators to fishing and environmental pressures},
volume = {70},
issn = {1054-3139, 1095-9289},
url = {http://icesjms.oxfordjournals.org/content/70/4/755},
doi = {10.1093/icesjms/fst067},
abstract = {Large, S. I., Fay, G., Friedland, K. D., and Link, J. S. 2013. Defining trends and thresholds in responses of ecological indicators to fishing and environmental pressures. – {ICES} Journal of Marine Science, 70: 755–767. Both fishing and environmental forces can influence the structure of marine ecosystems. To further understand marine ecosystems and to implement ecosystem-based fisheries management ({EBFM}), an evaluation of ecosystem indicators is warranted. In this context, it is particularly important to identify thresholds where fishing and environmental pressures significantly influence ecological indicators. We empirically determined numerical values of environmental forces and fishing pressure that significantly altered the response of ecological indicators for the Northeast Shelf Large Marine Ecosystem. Generalized additive models predicted a non-linear relationship for each pressure–response pairing. With this smoother, 95\% confidence intervals ({CI}) for estimated first and second derivatives for each relationship were determined via parametric bootstrap. A significant trend or threshold was noted when the {CI} for the first or second derivative was greater or less than zero, delineating the level at which pressure variables influence the rate and direction of ecosystem indicator responses. We identify reference levels where environmental forces and fishing pressure result in ecosystem change by collectively examining the responses of multiple ecological indicators. Individual indicators showed unique responses to pressures, however, similar values for the pressures were associated with significant changes for multiple indicators. These reference levels establish a foundation for implementation of {EBFM}.},
pages = {755--767},
number = {4},
journaltitle = {{ICES} Journal of Marine Science: Journal du Conseil},
shortjournal = {{ICES} J. Mar. Sci.},
author = {Large, Scott I. and Fay, Gavin and Friedland, Kevin D. and Link, Jason S.},
urldate = {2016-10-14},
date = {2013-07-01},
langid = {english},
keywords = {decision criteria, Ecosystem-based management, generalized additive model, overfishing, reference points},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\8JFINTNX\\Large et al. - 2013 - Defining trends and thresholds in responses of eco.pdf:application/pdf;Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\HHWWVVBA\\Large et al. - 2013 - Defining trends and thresholds in responses of eco.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\XDCNX8QE\\755.html:text/html;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\IHJNGJTU\\727721.html:text/html},
}
@article{miller_state-space_2016,
title = {A state-space approach to incorporating environmental effects on recruitment in an age-structured assessment model with an application to southern New England yellowtail flounder},
volume = {73},
issn = {0706-652X},
url = {https://www.nrcresearchpress.com/doi/10.1139/cjfas-2015-0339},
doi = {10.1139/cjfas-2015-0339},
abstract = {The state-space model framework provides a natural, probabilistic approach to stock assessment by modeling the stochastic nature of population survival and recruitment separately from sampling uncertainty inherent in observations on the population. We propose a state-space assessment model that is expanded to simultaneously treat environmental covariates as stochastic processes and estimate their effects on recruitment. We apply the model to southern New England yellowtail flounder (Limanda ferruginea) using data from the most recent benchmark assessment to evaluate evidence for effects of the mid-Atlantic cold pool and spawning stock biomass on recruitment. Based on Akaike’s information criterion, both the cold pool and spawning stock biomass were important predictors of recruitment and led to annual variation in estimated biomass reference points and associated yield. We also demonstrate the effect of the stochasticity of the mid-Atlantic cold pool on short-term forecasts of the stock size, biomass reference point, and stock status.},
pages = {1261--1270},
number = {8},
journaltitle = {Canadian Journal of Fisheries and Aquatic Sciences},
shortjournal = {Can. J. Fish. Aquat. Sci.},
author = {Miller, Timothy J. and Hare, Jonathan A. and Alade, Larry A.},
urldate = {2020-02-10},
date = {2016-02-10},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\22GJMCCS\\Miller et al. - 2016 - A state-space approach to incorporating environmen.pdf:application/pdf;NRC Research Press Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\GXGW3JES\\cjfas-2015-0339.html:text/html;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\LXNLXZIV\\cjfas-2015-0339.html:text/html},
}
@article{chen_seasonal_2018,
title = {Seasonal Variability of the Cold Pool Over the Mid-Atlantic Bight Continental Shelf},
volume = {123},
issn = {21699275},
url = {http://doi.wiley.com/10.1029/2018JC014148},
doi = {10.1029/2018JC014148},
abstract = {The Mid-Atlantic Bight ({MAB}) Cold Pool is a distinctive cold (lower than 10 ∘C) and relatively fresh (lower than 34 practical salinity unit) water mass. It is located over the middle and outer shelf of the {MAB}, below the seasonal thermocline, and is attached to the bottom. Following this definition, we put forward a method that includes three criteria to capture and quantify Cold Pool characteristics, based on a 50-year (1958–2007) high-resolution regional ocean model hindcast. The seasonal climatology of the Cold Pool and its properties are investigated during its onset-peak-decline cycle. Three stages of the Cold Pool event are defined according to its evolution and characteristics. The Cold Pool cores travel along the 60-m isobath starting south of the New England shelf to the Hudson Shelf Valley at a speed of 2–3 cm/s. Furthermore, the northern extent of the Cold Pool retreats about 2.6 times faster than the southern extent during the summer progression. The heat balance of near-bottom waters over the {MAB} and Georges Bank is computed and it is found that the heat advection, rather than vertical diffusion, dominates the resulting spatial patterns of warming. Possible origins of the Cold Pool are investigated by performing a lead-lag correlation analysis. Results suggest that the Cold Pool originates not only from local remnants of winter water near the Nantucket Shoals, but has an upstream source traveling in the spring time from the southwestern flank of the Georges Bank along the 80-m isobath.},
pages = {8203--8226},
number = {11},
journaltitle = {Journal of Geophysical Research: Oceans},
author = {Chen, Zhuomin and Curchitser, Enrique and Chant, Robert and Kang, Dujuan},
urldate = {2020-05-18},
date = {2018-11},
langid = {english},
file = {Chen et al. - 2018 - Seasonal Variability of the Cold Pool Over the Mid.pdf:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\YT6J2CZS\\Chen et al. - 2018 - Seasonal Variability of the Cold Pool Over the Mid.pdf:application/pdf},
}
@article{pdf,
title = {Optimization and assessment of phytoplankton size class algorithms for ocean color data on the Northeast U.S. continental shelf},
volume = {267},
issn = {0034-4257},
doi = {https://doi.org/10.1016/j.rse.2021.112729},
abstract = {The size structure of phytoplankton communities influences important ecological and biogeochemical processes, including the transfer of energy through marine food webs. A variety of algorithms have been developed to estimate phytoplankton size classes ({PSCs}) from satellite ocean color data. However, many of these algorithms were developed for application to the global ocean, and their performance in more productive, optically complex coastal and continental shelf regions warrants evaluation. In this study, several existing {PSC} models were applied in the Northeast U.S. continental shelf ({NES}) region and compared with in situ {PSC} estimates derived from a local {HPLC} pigment data set. The effect of regional re-parameterization and incorporation of sea surface temperature ({SST}) into existing abundance-based model frameworks was investigated and model performance was assessed using an independent data set. Abundance-based model re-parameterization alone did not result in significant improvement in model performance compared with other models. However, the inclusion of {SST} led to a consistent reduction in model error for all size classes. Of two absorption-based algorithms tested, the best performing approach displayed similar performance metrics to the regional {SST}-dependent abundance-based model. The {SST}-dependent model and the absorption-based method were applied to monthly composites of the {NES} region for April and September 2019 and qualitatively compared. The results highlight the benefit of considering {SST} in abundance-based models and the applicability of absorption-based {PSC} methods in optically complex regions.},
pages = {112729},
journaltitle = {Remote Sensing of Environment},
author = {Turner, Kyle J. and Mouw, Colleen B. and Hyde, Kimberly J. W. and Morse, Ryan and Ciochetto, Audrey B.},
date = {2021-12-15},
file = {Turner_etal-RSE_2021 Optimization and assessme:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\F6TA9NTB\\Turner_etal-RSE_2021 Optimization and assessme.pdf:application/pdf},
}
@article{pendleton_decadal-scale_2022,
title = {Decadal-scale phenology and seasonal climate drivers of migratory baleen whales in a rapidly warming marine ecosystem},
volume = {28},
rights = {© 2022 The Authors. Global Change Biology published by John Wiley \& Sons Ltd.},
issn = {1365-2486},
url = {https://onlinelibrary.wiley.com/doi/abs/10.1111/gcb.16225},
doi = {10.1111/gcb.16225},
abstract = {Species' response to rapid climate change can be measured through shifts in timing of recurring biological events, known as phenology. The Gulf of Maine is one of the most rapidly warming regions of the ocean, and thus an ideal system to study phenological and biological responses to climate change. A better understanding of climate-induced changes in phenology is needed to effectively and adaptively manage human-wildlife conflicts. Using data from a 20+ year marine mammal observation program, we tested the hypothesis that the phenology of large whale habitat use in Cape Cod Bay has changed and is related to regional-scale shifts in the thermal onset of spring. We used a multi-season occupancy model to measure phenological shifts and evaluate trends in the date of peak habitat use for North Atlantic right (Eubalaena glacialis), humpback (Megaptera novaeangliae), and fin (Balaenoptera physalus) whales. The date of peak habitat use shifted by +18.1 days (0.90 days/year) for right whales and +19.1 days (0.96 days/year) for humpback whales. We then evaluated interannual variability in peak habitat use relative to thermal spring transition dates ({STD}), and hypothesized that right whales, as planktivorous specialist feeders, would exhibit a stronger response to thermal phenology than fin and humpback whales, which are more generalist piscivorous feeders. There was a significant negative effect of western region {STD} on right whale habitat use, and a significant positive effect of eastern region {STD} on fin whale habitat use indicating differential responses to spatial seasonal conditions. Protections for threatened and endangered whales have been designed to align with expected phenology of habitat use. Our results show that whales are becoming mismatched with static seasonal management measures through shifts in their timing of habitat use, and they suggest that effective management strategies may need to alter protections as species adapt to climate change.},
pages = {4989--5005},
number = {16},
journaltitle = {Global Change Biology},
author = {Pendleton, Daniel E. and Tingley, Morgan W. and Ganley, Laura C. and Friedland, Kevin D. and Mayo, Charles and Brown, Moira W. and {McKenna}, Brigid E. and Jordaan, Adrian and Staudinger, Michelle D.},
urldate = {2024-02-02},
date = {2022},
langid = {english},
note = {\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16225},
keywords = {climate change, endangered species, fin whale, Gulf of Maine, humpback whale, North Atlantic right whale, ocean warming, phenology},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\U95ZX4Z7\\Pendleton et al. - 2022 - Decadal-scale phenology and seasonal climate drive.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\LTR2A577\\gcb.html:text/html},
}
@article{northeast_fisheries_science_center_us_state_2022,
title = {State of the Ecosystem 2022: Mid-Atlantic},
url = {https://repository.library.noaa.gov/view/noaa/38949},
doi = {10.25923/5S5Y-0H81},
shorttitle = {State of the Ecosystem 2022},
author = {Northeast Fisheries Science Center (U.S.)},
urldate = {2023-03-02},
date = {2022},
note = {Publisher: Northeast Fisheries Science Center (U.S.)},
}
@article{hernandez_seasonal_2019,
title = {Seasonal variability and individual consistency in gray seal (Halichoerus grypus) isotopic niches},
volume = {97},
issn = {0008-4301},
url = {https://cdnsciencepub.com/doi/10.1139/cjz-2019-0032},
doi = {10.1139/cjz-2019-0032},
abstract = {Although it is often assumed that individuals in generalist populations are equivalent, recent research indicates that individual dietary specialization can be common in marine predators. Gray seals (Halichoerus grypus (Fabricius, 1791)) were considered locally extinct in United States waters by 1958 but have since recolonized the region. Although considered generalists, less is known about gray seal foraging ecology in the United States. To address this, we used carbon and nitrogen stable isotope analyses to investigate the foraging niches of adult gray seals in Massachusetts, {USA}. We examined skin, fur, and blood components to investigate seasonal variability and individual consistency in foraging niches, and serially sampled vibrissae to quantify the degree of individual foraging specialization in this population. Our results suggest that seals shift from coastal foraging habitats before molt to offshore habitats after molt, with a coincident shift from higher to lower trophic-level prey. Adult gray seals also exhibited individual consistency in foraging niches independent of population-level shifts and reflect a generalist population composed of individual foraging specialists. These findings serve as a baseline for subsequent research on gray seals in United States waters that could help to determine the mechanisms which promote individual specialization in this population.},
pages = {1071--1077},
number = {11},
journaltitle = {Canadian Journal of Zoology},
shortjournal = {Can. J. Zool.},
author = {Hernandez, K.M. and Bogomolni, A.L. and Moxley, J.H. and Waring, G.T. and {DiGiovanni}, R.A. and Hammill, M.O. and Johnston, D.W. and Sette, L. and Polito, M.J.},
urldate = {2023-02-10},
date = {2019-11},
note = {Publisher: {NRC} Research Press},
}
@article{northeast_fisheries_science_center_us_state_2022-1,
title = {State of the Ecosystem 2022: New England},
url = {https://repository.library.noaa.gov/view/noaa/38948},
doi = {10.25923/YPV2-MW79},
shorttitle = {State of the Ecosystem 2022},
author = {Northeast Fisheries Science Center (U.S.)},
urldate = {2023-03-02},
date = {2022},
note = {Publisher: Northeast Fisheries Science Center (U.S.)},
}
@article{fabrizio_characterization_2022,
title = {Characterization of Nursery Habitats used by Black Sea Bass and Summer Flounder in Chesapeake Bay and the Coastal Lagoons},
url = {https://scholarworks.wm.edu/reports/2837},
doi = {doi: 10.25773/PJCC-RG41},
journaltitle = {Reports},
author = {Fabrizio, Mary and Tuckey, Troy and Smith, Shannon and Ross, Paige and Snyder, Richard and Wang, Harry and Bever, Aaron},
date = {2022-01-01},
file = {"Characterization of Nursery Habitats used by Black Sea Bass and Summer" by Mary C. Fabrizio, Troy D. Tuckey et al.:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\Z39AE9UV\\2837.html:text/html},
}
@article{mccosker_metabarcoding_2020,
title = {Metabarcoding Fecal {DNA} Reveals Extent of Halichoerus grypus (Gray Seal) Foraging on Invertebrates and Incidence of Parasite Exposure},
volume = {27},
issn = {1092-6194, 1938-5307},
url = {https://bioone.org/journals/northeastern-naturalist/volume-27/issue-4/045.027.0409/Metabarcoding-Fecal-DNA-Reveals-Extent-of-Halichoerus-grypus-Gray-Seal/10.1656/045.027.0409.full},
doi = {10.1656/045.027.0409},
abstract = {Halichoerus grypus (Gray Seal) is a top predator in New England waters, yet little data exists on seals foraging on invertebrate prey. We combined analysis of hard parts of scat samples (n = 98) from 2 breeding sites in Massachusetts with metabarcoding of fecal {DNA}. Invertebrates were detected in 4 samples via analysis of hard parts (4.1\%) but in 35 samples (35.7\%) using a metabarcoding approach. Metabarcoding also detected parasite {DNA} in 82.7\% of scat samples. Nematode {DNA} (78.6\%) was more prevalent than trematode (28.6\%) or cestode (22.5\%) {DNA}. Prey species, biomass, and diversity within each sample were not affected by seal sex, parasite exposure, or type of parasitic exposure. Previous diet studies may have underestimated the diversity and abundance of invertebrates in the diet of Gray Seals.},
pages = {681--700},
number = {4},
journaltitle = {Northeastern Naturalist},
shortjournal = {nena},
author = {{McCosker}, Christina and Flanders, Kelly and Ono, Kathryn and Dufault, Michelle and Mellone, Dominique and Olson, Zachary},
urldate = {2023-02-10},
date = {2020-11},
note = {Publisher: Eagle Hill Institute},
}
@article{ono_detecting_2019,
title = {Detecting spiny dogfish in grey seal diets},
volume = {11},
issn = {1877-7260},
url = {https://doi.org/10.1007/s12686-018-1044-x},
doi = {10.1007/s12686-018-1044-x},
abstract = {Grey seal (Halichoerus grypus) populations declined dramatically in U.S. waters during the nineteenth and twentieth centuries, but have rebounded in recent decades as a result of legal protection. In the Gulf of Maine, increasing grey seal populations have the potential to impact commercially important groundfish species such as cod and haddock, but the potential also exists for more complex ecological interactions to occur given the recent increase of spiny dogfish (Squalus acanthias), another potential groundfish predator. Specifically, seal predation on dogfish could free groundfish species from additional predation pressure. Little quantitative data exists on intraguild predation rates by grey seals on spiny dogfish, in part because of the limitations of current methods of food habits analysis for grey seals. We report the development, validation, and field testing of a non-invasive genetic method for the detection of spiny dogfish in grey seal diets using {DNA} collected from seal feces. Our method amplified spiny dogfish {DNA} from 10 of 10 positive control scats from a captive seal with a known diet, and amplified spiny dogfish {DNA} from 0 of 10 negative control scats. We field tested the method on 20 scats from wild seals and detected spiny dogfish in two of the samples. All positive amplifications were sequenced to verify the species identify, and all were spiny dogfish. Our method has the potential to provide valuable information about changing predator prey dynamics in the Gulf of Maine and elsewhere.},
pages = {481--485},
number = {4},
journaltitle = {Conservation Genetics Resources},
shortjournal = {Conservation Genet Resour},
author = {Ono, Kathryn A. and Steinbeiser, Cathleen M. and Coco, Austin B. and Sheehan, Matthew J. and Beck, Abigail J. and Dufault, Michelle N. and Gilbert, Katelyn M. and Antonez, Jessica J. and Olson, Zachary H.},
urldate = {2023-02-10},
date = {2019-12-01},
langid = {english},
}
@article{flanders_utilizing_2020,
title = {Utilizing next-generation sequencing to identify prey {DNA} in western North Atlantic grey seal Halichoerus grypus diet},
volume = {655},
issn = {0171-8630, 1616-1599},
url = {https://www.int-res.com/abstracts/meps/v655/p227-240/},
doi = {10.3354/meps13520},
abstract = {Increasing grey seal Halichoerus grypus abundance in coastal New England is leading to social, political, economic, and ecological controversies. Central to these issues is the foraging ecology and diet composition of the seals. We studied grey seal feeding habits through next-generation sequencing of prey {DNA} using 16S amplicons from seal scat (n = 74) collected from a breeding colony on Monomoy Island in Massachusetts, {USA}, and report frequency of occurrence and relative read abundance. We also assigned seal sex to scat samples using a revised {PCR} assay. In contrast to current understanding of grey seal diet from hard parts and fatty acid analysis, we found no significant difference between male and female diet measured by alpha and beta diversity. Overall, we detected 24 prey groups, 18 of which resolved to species. Sand lance Ammodytes spp. were the most frequently consumed prey group, with a frequency of occurrence ({FO}) of 97.3\%, consistent with previous studies, but Atlantic menhaden Brevoortia tyrannus, the second most frequently consumed species ({FO} = 60.8\%), has not previously been documented in {US} grey seal diet. Our results suggest that a metabarcoding approach to seal food habits can yield important new ecological insights, but that traditional hard parts analysis does not underestimate consumption of Atlantic cod Gadus morhua ({FO} = 6.7\%, Gadidae spp.) and salmon Salmo salar ({FO} = 0\%), 2 particularly valuable species of concern.},
pages = {227--240},
journaltitle = {Marine Ecology Progress Series},
author = {Flanders, Kelly R. and Olson, Zachary H. and Ono, Kathryn A.},
urldate = {2023-02-10},
date = {2020-11-26},
langid = {english},
keywords = {Diet, Foraging ecology, Grey seal, Halichoerus grypus, Molecular scatology, Next-generation sequencing, Prey {DNA}},
}
@article{saba_recommended_2019,
title = {Recommended priorities for research on ecological impacts of ocean and coastal acidification in the U.S. Mid-Atlantic},
volume = {225},
issn = {0272-7714},
url = {https://www.sciencedirect.com/science/article/pii/S0272771418308710},
doi = {10.1016/j.ecss.2019.04.022},
abstract = {The estuaries and continental shelf system of the United States Mid-Atlantic are subject to ocean acidification driven by atmospheric {CO}2, and coastal acidification caused by nearshore and land-sea interactions that include biological, chemical, and physical processes. These processes include freshwater and nutrient input from rivers and groundwater; tidally-driven outwelling of nutrients, inorganic carbon, alkalinity; high productivity and respiration; and hypoxia. Hence, these complex dynamic systems exhibit substantial daily, seasonal, and interannual variability that is not well captured by current acidification research on Mid-Atlantic organisms and ecosystems. We present recommendations for research priorities that target better understanding of the ecological impacts of acidification in the U. S. Mid-Atlantic region. Suggested priorities are: 1) Determining the impact of multiple stressors on our resource species as well as the magnitude of acidification; 2) Filling information gaps on major taxa and regionally important species in different life stages to improve understanding of their response to variable temporal scales and sources of acidification; 3) Improving experimental approaches to incorporate realistic environmental variability and gradients, include interactions with other environmental stressors, increase transferability to other systems or organisms, and evaluate community and ecosystem response; 4) Determining the capacity of important species to acclimate or adapt to changing ocean conditions; 5) Considering multi-disciplinary, ecosystem-level research that examines acidification impacts on biodiversity and biotic interactions; and 6) Connecting potential acidification-induced ecological impacts to ecosystem services and the economy. These recommendations, while developed for the Mid-Atlantic, can be applicable to other regions will help align research towards knowledge of potential larger-scale ecological and economic impacts.},
pages = {106188},
journaltitle = {Estuarine, Coastal and Shelf Science},
shortjournal = {Estuarine, Coastal and Shelf Science},
author = {Saba, Grace K. and Goldsmith, Kaitlin A. and Cooley, Sarah R. and Grosse, Daniel and Meseck, Shannon L. and Miller, A. Whitman and Phelan, Beth and Poach, Matthew and Rheault, Robert and St.Laurent, Kari and Testa, Jeremy M. and Weis, Judith S. and Zimmerman, Richard},
urldate = {2023-02-10},
date = {2019-09-30},
langid = {english},
file = {ScienceDirect Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\CH36QAJB\\Saba et al. - 2019 - Recommended priorities for research on ecological .pdf:application/pdf;ScienceDirect Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\SAP7FLGR\\S0272771418308710.html:text/html},
}
@article{zakroff_antagonistic_2020,
title = {Antagonistic Interactions and Clutch-Dependent Sensitivity Induce Variable Responses to Ocean Acidification and Warming in Squid (Doryteuthis pealeii) Embryos and Paralarvae},
volume = {11},
issn = {1664-042X},
url = {https://www.frontiersin.org/articles/10.3389/fphys.2020.00501},
abstract = {Ocean acidification ({OA}) and warming seas are significant concerns for coastal systems and species. The Atlantic longfin squid, Doryteuthis pealeii, a core component of the Northwest Atlantic trophic web, has demonstrated impacts, such as reduced growth and delayed development, under high chronic exposure to acidification (2200 ppm), but the combined effects of {OA} and warming have not been explored in this species. In this study, D. pealeii egg capsules were reared under a combination of several acidification levels (400, 2200, and 3500 ppm) and temperatures (20 and 27°C). Hatchlings were measured for a range of metrics [dorsal mantle length ({DML}), yolk sac volume ({YV}), malformation, and hatching success] in three trials over the 2016 breeding season (May – October). Although notable resistance to stressors was seen, highlighting variability within and between clutches, reduced {DML} and malformation of the embryos occurred at the highest {OA} exposure. Surprisingly, increased temperatures did not appear to exacerbate {OA} impacts, although responses were variable. Time to hatching, which increased with acidification, decreased much more drastically under warming and, further, decreased or removed delays caused by acidification. Hatching success, while variable by clutch, showed consistent patterns of greater late stage loss of embryos under acidification and greater early stage loss under warming, highlighting the potential difference in timing between these stressors for this system, i.e., that acidification stress builds up and causes impacts over time within the egg capsule as the embryos grow and respire. High {OA}-exposed hatchlings from the warmer conditions often showed reduced impacts compared to those reared in ambient temperatures. This may be due to the increased developmental rate and subsequently reduced {OA} exposure time of embryos in the higher temperature treatment. These results indicate a substantive potential plasticity to multiple stressors during the embryonic development of this species of squid, but do not predict how this species would fare under these future ocean scenarios.},
journaltitle = {Frontiers in Physiology},
author = {Zakroff, Casey J. and Mooney, T. Aran},
urldate = {2023-02-09},
date = {2020},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\IIG335QG\\Zakroff and Mooney - 2020 - Antagonistic Interactions and Clutch-Dependent Sen.pdf:application/pdf},
}
@article{chavez-rosales_detection_2022,
title = {Detection of Habitat Shifts of Cetacean Species: A Comparison Between 2010 and 2017 Habitat Suitability Conditions in the Northwest Atlantic Ocean},
volume = {9},
issn = {2296-7745},
url = {https://www.frontiersin.org/articles/10.3389/fmars.2022.877580},
shorttitle = {Detection of Habitat Shifts of Cetacean Species},
abstract = {The simultaneous effects of human activities in the ocean and climate change have already produced a series of responses from the marine ecosystems. With the potential increment of future human activities, such as offshore renewable energy developments, proactive management is required. To facilitate effective management and conservation actions, it is imperative to identify species potentially at risk and their critical habitats. Here we examine 16 cetacean species habitat suitability in the western North Atlantic Ocean using generalized additive models developed from data collected by {NOAA}- Northeast and Southeast Fisheries Science Centers from 2010 to 2017. The models were based on observed species distribution as a function of 21 environmental covariates and compare species-specific core habitats between 2010 and 2017. We identified seasonal differences in patterns of habitat change across guilds and an average northward shift of 178 km across the study area. The effects of these shifts are still unknown, but for already stressed species, the contraction or displacement of their historical habitat could worsen their population status. Therefore, the imminent development of offshore regions, in addition to the effects of climate change emphasize the need of adaptively managing ecosystems on the face of multiple challenges.},
journaltitle = {Frontiers in Marine Science},
author = {Chavez-Rosales, Samuel and Josephson, Elizabeth and Palka, Debra and Garrison, Lance},
urldate = {2023-02-09},
date = {2022},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\CVGTYCW6\\Chavez-Rosales et al. - 2022 - Detection of Habitat Shifts of Cetacean Species A.pdf:application/pdf},
}
@article{zakroff_dose-dependence_2019,
title = {Dose-dependence and small-scale variability in responses to ocean acidification during squid, Doryteuthis pealeii, development},
volume = {166},
issn = {1432-1793},
url = {https://doi.org/10.1007/s00227-019-3510-8},
doi = {10.1007/s00227-019-3510-8},
abstract = {Coastal squids lay their eggs on the benthos, leaving them to develop in a dynamic system that is undergoing rapid acidification due to human influence. Prior studies have broadly investigated the impacts of ocean acidification on embryonic squid, but have not addressed the thresholds at which these responses occur or their potential variability. We raised squid, Doryteuthis pealeii (captured in Vineyard Sound, Massachusetts, {USA}: 41°23.370'N 70°46.418′W), eggs in three trials across the breeding season (May–September, 2013) in a total of six chronic {pCO}2 exposures (400, 550, 850, 1300, 1900, and 2200 ppm). Hatchlings were counted and subsampled for mantle length, yolk volume, hatching time, hatching success, and statolith morphology. New methods for analysis of statolith shape, rugosity, and surface degradation were developed and are presented (with code). Responses to acidification (e.g., reduced mantle lengths, delayed hatching, and smaller, more degraded statoliths) were evident at {\textasciitilde} 1300 ppm {CO}2. However, patterns of physiological response and energy management, based on comparisons of yolk consumption and growth, varied among trials. Interactions between {pCO}2 and hatching day indicated a potential influence of exposure time on responses, while interactions with culture vessel highlighted the substantive natural variability within a clutch of eggs. While this study is consistent with, and expands upon, previous findings of sensitivity of the early life stages to acidification, it also highlights the plasticity and potential for resilience in this population of squid.},
pages = {62},
number = {5},
journaltitle = {Marine Biology},
shortjournal = {Mar Biol},
author = {Zakroff, Casey and Mooney, T. Aran and Berumen, Michael L.},
urldate = {2023-02-09},
date = {2019-04-19},
langid = {english},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\GR29VF7U\\Zakroff et al. - 2019 - Dose-dependence and small-scale variability in res.pdf:application/pdf},
}
@article{cameron_effects_2022,
title = {Effects of elevated {pCO}2 and temperature on the calcification rate, survival, extrapallial fluid chemistry, and respiration of the Atlantic Sea scallop Placopecten magellanicus},
volume = {67},
issn = {1939-5590},
url = {https://onlinelibrary.wiley.com/doi/abs/10.1002/lno.12153},
doi = {10.1002/lno.12153},
abstract = {Anthropogenic {CO}2-emission is causing ocean warming and acidification. Understanding how basic physiological processes of marine organisms respond to these stressors is important for predicting their responses to future global change. We examined the effects of elevated {pCO}2 and temperature ({pCO}2 = 344–2199 ppm; temperature = 6°C, 9°C, and 12°C) on the calcification rate, extrapallial fluid ({EPF}) carbonate chemistry, respiration, and survivorship of Atlantic sea scallops (Placopecten magellanicus) in a fully crossed 143-d experiment. Rates of calcification and respiration were inhibited by elevated {pCO}2, and mortality occurred when elevated {pCO}2 was accompanied by high-temperature stress. Declines in growth and survivorship were likely caused by external shell dissolution, thermal stress, and hypercapnic reduction of metabolism under elevated {pCO}2. Concentrations of dissolved inorganic carbon ({DIC}) and total alkalinity in the {EPF} increased above seawater concentrations in response to elevated {pCO}2. {EPF} {pH} declined, but did not decline as much as seawater {pH}, indicating that scallops regulate {EPF} {pH} to support calcification. The combination of {EPF} {pH} regulation and {DIC} elevation yielded an increase in {EPF} [{CO}32−] under elevated {pCO}2 treatments. The combination of low respiration rates, high {EPF} [{CO}32−], and low calcification rates under elevated {pCO}2 suggests that the impaired calcification arises more from hypercapnic inhibition of metabolic activity and external shell dissolution than from chemically unfavorable conditions in the {EPF}. These results demonstrate the importance of {EPF} chemistry for bivalve biomineralization, but show that regulation efforts are insufficient to fully offset the deleterious effects of elevated {pCO}2 on scallop performance.},
pages = {1670--1686},
number = {8},
journaltitle = {Limnology and Oceanography},
author = {Cameron, Louise P. and Grabowski, Jonathan H. and Ries, Justin B.},
urldate = {2023-02-09},
date = {2022},
langid = {english},
note = {\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.12153},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\YYPRLBMB\\Cameron et al. - 2022 - Effects of elevated pCO2 and temperature on the ca.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\R9LYV4DJ\\lno.html:text/html},
}
@article{kroeker_impacts_2013,
title = {Impacts of ocean acidification on marine organisms: quantifying sensitivities and interaction with warming},
volume = {19},
issn = {1365-2486},
url = {https://onlinelibrary.wiley.com/doi/abs/10.1111/gcb.12179},
doi = {10.1111/gcb.12179},
shorttitle = {Impacts of ocean acidification on marine organisms},
abstract = {Ocean acidification represents a threat to marine species worldwide, and forecasting the ecological impacts of acidification is a high priority for science, management, and policy. As research on the topic expands at an exponential rate, a comprehensive understanding of the variability in organisms' responses and corresponding levels of certainty is necessary to forecast the ecological effects. Here, we perform the most comprehensive meta-analysis to date by synthesizing the results of 228 studies examining biological responses to ocean acidification. The results reveal decreased survival, calcification, growth, development and abundance in response to acidification when the broad range of marine organisms is pooled together. However, the magnitude of these responses varies among taxonomic groups, suggesting there is some predictable trait-based variation in sensitivity, despite the investigation of approximately 100 new species in recent research. The results also reveal an enhanced sensitivity of mollusk larvae, but suggest that an enhanced sensitivity of early life history stages is not universal across all taxonomic groups. In addition, the variability in species' responses is enhanced when they are exposed to acidification in multi-species assemblages, suggesting that it is important to consider indirect effects and exercise caution when forecasting abundance patterns from single-species laboratory experiments. Furthermore, the results suggest that other factors, such as nutritional status or source population, could cause substantial variation in organisms' responses. Last, the results highlight a trend towards enhanced sensitivity to acidification when taxa are concurrently exposed to elevated seawater temperature.},
pages = {1884--1896},
number = {6},
journaltitle = {Global Change Biology},
author = {Kroeker, Kristy J. and Kordas, Rebecca L. and Crim, Ryan and Hendriks, Iris E. and Ramajo, Laura and Singh, Gerald S. and Duarte, Carlos M. and Gattuso, Jean-Pierre},
urldate = {2023-02-09},
date = {2013},
langid = {english},
note = {\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.12179},
keywords = {climate change, calcification, carbonate chemistry, cumulative effects, {pH}},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\DYRRBCYG\\Kroeker et al. - 2013 - Impacts of ocean acidification on marine organisms.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\CX69QCAH\\gcb.html:text/html},
}
@incollection{intergovernmental_panel_on_climate_change_ipcc_technical_2022,
location = {Cambridge},
title = {Technical Summary},
isbn = {978-1-00-915796-4},
url = {https://www.cambridge.org/core/books/ocean-and-cryosphere-in-a-changing-climate/technical-summary/3428BF3C6ADE0C52755DBC3AA5CFE48B},
pages = {39--70},
booktitle = {The Ocean and Cryosphere in a Changing Climate: Special Report of the Intergovernmental Panel on Climate Change},
publisher = {Cambridge University Press},
editor = {{Intergovernmental Panel on Climate Change (IPCC)}},
urldate = {2023-02-09},
date = {2022},
doi = {10.1017/9781009157964.002},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\HHCSDHSB\\Intergovernmental Panel on Climate Change (IPCC) - 2022 - Technical Summary.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\GRTJWG2H\\3428BF3C6ADE0C52755DBC3AA5CFE48B.html:text/html},
}
@article{cheng_another_2023,
title = {Another Year of Record Heat for the Oceans},
issn = {1861-9533},
url = {https://doi.org/10.1007/s00376-023-2385-2},
doi = {10.1007/s00376-023-2385-2},
abstract = {Changes in ocean heat content ({OHC}), salinity, and stratification provide critical indicators for changes in Earth’s energy and water cycles. These cycles have been profoundly altered due to the emission of greenhouse gasses and other anthropogenic substances by human activities, driving pervasive changes in Earth’s climate system. In 2022, the world’s oceans, as given by {OHC}, were again the hottest in the historical record and exceeded the previous 2021 record maximum. According to {IAP}/{CAS} data, the 0–2000 m {OHC} in 2022 exceeded that of 2021 by 10.9 ± 8.3 {ZJ} (1 Zetta Joules = 1021 Joules); and according to {NCEI}/{NOAA} data, by 9.1 ± 8.7 {ZJ}. Among seven regions, four basins (the North Pacific, North Atlantic, the Mediterranean Sea, and southern oceans) recorded their highest {OHC} since the 1950s. The salinity-contrast index, a quantification of the “salty gets saltier—fresh gets fresher” pattern, also reached its highest level on record in 2022, implying continued amplification of the global hydrological cycle. Regional {OHC} and salinity changes in 2022 were dominated by a strong La Niña event. Global upper-ocean stratification continued its increasing trend and was among the top seven in 2022.},
journaltitle = {Advances in Atmospheric Sciences},
shortjournal = {Adv. Atmos. Sci.},
author = {Cheng, Lijing and Abraham, John and Trenberth, Kevin E. and Fasullo, John and Boyer, Tim and Mann, Michael E. and Zhu, Jiang and Wang, Fan and Locarnini, Ricardo and Li, Yuanlong and Zhang, Bin and Yu, Fujiang and Wan, Liying and Chen, Xingrong and Feng, Licheng and Song, Xiangzhou and Liu, Yulong and Reseghetti, Franco and Simoncelli, Simona and Gouretski, Viktor and Chen, Gengxin and Mishonov, Alexey and Reagan, Jim and Li, Guancheng},
urldate = {2023-02-09},
date = {2023-01-11},
langid = {english},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\Q3V76Y9J\\Cheng et al. - 2023 - Another Year of Record Heat for the Oceans.pdf:application/pdf},
}
@article{northeast_fisheries_science_center_us_noaa_2022,
title = {{NOAA} Fisheries and {BOEM} Federal Survey Mitigation Implementation Strategy - Northeast U.S. Region},
url = {https://repository.library.noaa.gov/view/noaa/47925},
doi = {10.25923/jqse-x746},
series = {{NOAA} technical memorandum {NMFS}-{NE} ; 292},
abstract = {This Federal Survey Mitigation Strategy (hereafter Strategy) is intended to guide the development and implementation of a program to mitigate impacts of wind energy development on fisheries surveys over the expected full duration (30+ years) of wind energy development in the Northeast U.S. (Mitigation Program). The Mitigation Program will include survey-specific mitigation plans for each impacted survey, including both vessel and aerial surveys (Survey Specific Mitigation Plans). This strategy is specific to the Northeast U.S. Region (Maine to North Carolina) and generally applicable to other regions of the country.},
author = {Hare, J.A. and Blythe, B.J. and Ford, K.H. and Godfrey-McKee, S. and Hooker, B.R. and Jensen, B.M. and Lipsky, A. and Nachman, C. and Pfeiffer, L. and Rasser, M. and Renshaw, K.},
editor = {{Northeast Fisheries Science Center (U.S.)}},
date = {2022},
keywords = {Effect of wind power plants on, Fish surveys},
}
@article{pousse_dynamic_2022,
title = {Dynamic energy budget modeling of Atlantic surfclam, Spisula solidissima, under future ocean acidification and warming},
volume = {177},
issn = {0141-1136},
url = {https://www.sciencedirect.com/science/article/pii/S0141113622000472},
doi = {10.1016/j.marenvres.2022.105602},
abstract = {A dynamic energy budget ({DEB}) model integrating {pCO}2 was used to describe ocean acidification ({OA}) effects on Atlantic surfclam, Spisula solidissima, bioenergetics. Effects of elevated {pCO}2 on ingestion and somatic maintenance costs were simulated, validated, and adapted in the {DEB} model based upon growth and biological rates acquired during a 12-week laboratory experiment. Temperature and {pCO}2 were projected for the next 100 years following the intergovernmental panel on climate change representative concentration pathways scenarios (2.6, 6.0, and 8.5) and used as forcing variables to project surfclam growth and reproduction. End-of-century water warming and acidification conditions resulted in simulated faster growth for young surfclams and more energy allocated to reproduction until the beginning of the 22nd century when a reduction in maximum shell length and energy allocated to reproduction was observed for the {RCP} 8.5 scenario.},
pages = {105602},
journaltitle = {Marine Environmental Research},
shortjournal = {Marine Environmental Research},
author = {Pousse, Émilien and Munroe, Daphne and Hart, Deborah and Hennen, Daniel and Cameron, Louise P. and Rheuban, Jennie E. and Wang, Zhaohui Aleck and Wikfors, Gary H. and Meseck, Shannon L.},
urldate = {2023-02-07},
date = {2022-05-01},
langid = {english},
keywords = {Atlantic surfclam, Climate change, Dynamic energy budget, Ocean acidification},
file = {ScienceDirect Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\82SNY4Q3\\S0141113622000472.html:text/html},
}
@article{jacox_global_2022,
title = {Global seasonal forecasts of marine heatwaves},
volume = {604},
rights = {2022 This is a U.S. government work and not under copyright protection in the U.S.; foreign copyright protection may apply},
issn = {1476-4687},
url = {https://www.nature.com/articles/s41586-022-04573-9},
doi = {10.1038/s41586-022-04573-9},
abstract = {Marine heatwaves ({MHWs})—periods of exceptionally warm ocean temperature lasting weeks to years—are now widely recognized for their capacity to disrupt marine ecosystems1–3. The substantial ecological and socioeconomic impacts of these extreme events present significant challenges to marine resource managers4–7, who would benefit from forewarning of {MHWs} to facilitate proactive decision-making8–11. However, despite extensive research into the physical drivers of {MHWs}11,12, there has been no comprehensive global assessment of our ability to predict these events. Here we use a large multimodel ensemble of global climate forecasts13,14 to develop and assess {MHW} forecasts that cover the world’s oceans with lead times of up to a year. Using 30 years of retrospective forecasts, we show that the onset, intensity and duration of {MHWs} are often predictable, with skilful forecasts possible from 1 to 12 months in advance depending on region, season and the state of large-scale climate modes, such as the El Niño/Southern Oscillation. We discuss considerations for setting decision thresholds based on the probability that a {MHW} will occur, empowering stakeholders to take appropriate actions based on their risk profile. These results highlight the potential for operational {MHW} forecasts, analogous to forecasts of extreme weather phenomena, to promote climate resilience in global marine ecosystems.},
pages = {486--490},
number = {7906},
journaltitle = {Nature},
author = {Jacox, Michael G. and Alexander, Michael A. and Amaya, Dillon and Becker, Emily and Bograd, Steven J. and Brodie, Stephanie and Hazen, Elliott L. and Pozo Buil, Mercedes and Tommasi, Desiree},
urldate = {2023-02-07},
date = {2022-04},
langid = {english},
note = {Number: 7906
Publisher: Nature Publishing Group},
keywords = {Natural hazards, Physical oceanography},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\UUUPVNQR\\Jacox et al. - 2022 - Global seasonal forecasts of marine heatwaves.pdf:application/pdf},
}
@article{jacox_thermal_2020,
title = {Thermal displacement by marine heatwaves},
volume = {584},
rights = {2020 The Author(s), under exclusive licence to Springer Nature Limited},
issn = {1476-4687},
url = {https://www.nature.com/articles/s41586-020-2534-z},
doi = {10.1038/s41586-020-2534-z},
abstract = {Marine heatwaves ({MHWs})—discrete but prolonged periods of anomalously warm ocean temperatures—can drastically alter ocean ecosystems, with profound ecological and socioeconomic impacts1–8. Considerable effort has been directed at understanding the patterns, drivers and trends of {MHWs} globally9–11. Typically, {MHWs} are characterized on the basis of their intensity and persistence at a given location—an approach that is particularly relevant for corals and other sessile organisms that must endure increased temperatures. However, many ecologically and commercially important marine species respond to environmental disruptions by relocating to favourable habitats, and dramatic range shifts of mobile marine species are among the conspicuous impacts of {MHWs}1,4,12,13. Whereas spatial temperature shifts have been studied extensively in the context of long-term warming trends14–18, they are unaccounted for in existing global {MHW} analyses. Here we introduce thermal displacement as a metric that characterizes {MHWs} by the spatial shifts of surface temperature contours, instead of by local temperature anomalies, and use an observation-based global sea surface temperature dataset to calculate thermal displacements for all {MHWs} from 1982 to 2019. We show that thermal displacements during {MHWs} vary from tens to thousands of kilometres across the world’s oceans and do not correlate spatially with {MHW} intensity. Furthermore, short-term thermal displacements during {MHWs} are of comparable magnitude to century-scale shifts inferred from warming trends18, although their global spatial patterns are very different. These results expand our understanding of {MHWs} and their potential impacts on marine species, revealing which regions are most susceptible to thermal displacement, and how such shifts may change under projected ocean warming. The findings also highlight the need for marine resource management to account for {MHW}-driven spatial shifts, which are of comparable scale to those associated with long-term climate change and are already happening.},
pages = {82--86},
number = {7819},
journaltitle = {Nature},
author = {Jacox, Michael G. and Alexander, Michael A. and Bograd, Steven J. and Scott, James D.},
urldate = {2023-02-07},
date = {2020-08},
langid = {english},
note = {Number: 7819
Publisher: Nature Publishing Group},
keywords = {Natural hazards, Physical oceanography, Environmental health},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\ZCEBPKE5\\Jacox et al. - 2020 - Thermal displacement by marine heatwaves.pdf:application/pdf},
}
@article{jiang_climatological_2015,
title = {Climatological distribution of aragonite saturation state in the global oceans},
volume = {29},
issn = {1944-9224},
url = {https://onlinelibrary.wiley.com/doi/abs/10.1002/2015GB005198},
doi = {10.1002/2015GB005198},
abstract = {Aragonite saturation state (Ωarag) in surface and subsurface waters of the global oceans was calculated from up-to-date (through the year of 2012) ocean station dissolved inorganic carbon ({DIC}) and total alkalinity ({TA}) data. Surface Ωarag in the open ocean was always supersaturated (Ω {\textgreater} 1), ranging between 1.1 and 4.2. It was above 2.0 (2.0–4.2) between 40°N and 40°S but decreased toward higher latitude to below 1.5 in polar areas. The influences of water temperature on the {TA}/{DIC} ratio, combined with the temperature effects on inorganic carbon equilibrium and apparent solubility product (K′sp), explain the latitudinal differences in surface Ωarag. Vertically, Ωarag was highest in the surface mixed layer. Higher hydrostatic pressure, lower water temperature, and more {CO}2 buildup from biological activity in the absence of air-sea gas exchange helped maintain lower Ωarag in the deep ocean. Below the thermocline, aerobic decomposition of organic matter along the pathway of global thermohaline circulation played an important role in controlling Ωarag distributions. Seasonally, surface Ωarag above 30° latitudes was about 0.06 to 0.55 higher during warmer months than during colder months in the open-ocean waters of both hemispheres. Decadal changes of Ωarag in the Atlantic and Pacific Oceans showed that Ωarag in waters shallower than 100 m depth decreased by 0.10 ± 0.09 (−0.40 ± 0.37\% yr−1) on average from the decade spanning 1989–1998 to the decade spanning 1998–2010.},
pages = {1656--1673},
number = {10},
journaltitle = {Global Biogeochemical Cycles},
author = {Jiang, Li-Qing and Feely, Richard A. and Carter, Brendan R. and Greeley, Dana J. and Gledhill, Dwight K. and Arzayus, Krisa M.},
urldate = {2023-02-06},
date = {2015},
langid = {english},
note = {\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015GB005198},
keywords = {{pH}, aragonite saturation state, climatology, global oceans, ocean acidification, omega},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\4YWKM4FH\\Jiang et al. - 2015 - Climatological distribution of aragonite saturatio.pdf:application/pdf;Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\ANLLFDHC\\Jiang et al. - 2015 - Climatological distribution of aragonite saturatio.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\UHSW7LKY\\2015GB005198.html:text/html},
}
@article{frick_spatiotemporal_2022,
title = {Spatiotemporal Variation in Distribution, Size, and Relative Abundance within a Salish Sea Nearshore Forage Fish Community},
volume = {14},
issn = {1942-5120},
url = {https://onlinelibrary.wiley.com/doi/abs/10.1002/mcf2.10202},
doi = {10.1002/mcf2.10202},
abstract = {Forage fish are schooling species commonly occurring in both offshore pelagic and nearshore coastal habitats. Beyond use by some species for spawning, the dynamics of nearshore habitat use are not well understood. The objective of our study was to evaluate the spring–summer dynamics of forage fish occurrence in nearshore habitats of the Strait of Juan de Fuca, Washington. We suspected that habitat changes resulting from removal of two large dams on the Elwha River (2009–2011) may have altered fish presence and abundance. Monthly beach seine sampling in four regions along 40 km of shoreline was conducted from April to September between 2006 and 2019. We caught nearly 600,000 fish, comprising 82 different species. Nine species of forage fish accounted for 81.7\% of all fishes caught; most were classified as postlarvae and juveniles based on size. There were spatial differences in the forage fish assemblage between two of our sites but no discernable year effects and no obvious impact of dam removal on forage community composition. Three species represented 78.8\% of the catch: Pacific Herring Clupea pallasii, Pacific Sand Lance Ammodytes hexapterus, and Surf Smelt Hypomesus pretiosus. We used a Bayesian generalized linear mixed model to evaluate spatial and temporal variability in the probability of occurrence of these species. Each species exhibited a unique pattern of intra-annual, interannual, and regional fluctuations. Pacific Herring occurrence progressively increased monthly, Pacific Sand Lance occurrence decreased, and Surf Smelt probability of occurrence peaked in June. Temporal variations in distribution and abundance of these species are likely driven by life history differences and biological requirements. We speculate that specific characteristics of each region, including proximity to spawning areas, spawn timing, extant current patterns, and ecosystem processes, drove variations in distribution between species.},
pages = {e10202},
number = {2},
journaltitle = {Marine and Coastal Fisheries},
author = {Frick, Kinsey E. and Kagley, Anna N. and Fresh, Kurt L. and Samhouri, Jameal F. and Ward, Larry S. and Stapleton, Justin T. and Shelton, Andrew O.},
urldate = {2023-01-30},
date = {2022},
langid = {english},
note = {\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/mcf2.10202},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\DVX64IVC\\Frick et al. - 2022 - Spatiotemporal Variation in Distribution, Size, an.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\G39AQAUN\\mcf2.html:text/html},
}
@article{schonfeld_spatial_2022,
title = {Spatial differences in estuarine utilization by seasonally resident species in Mid-Atlantic Bight, {USA}},
volume = {31},
issn = {1365-2419},
url = {https://onlinelibrary.wiley.com/doi/abs/10.1111/fog.12611},
doi = {10.1111/fog.12611},
abstract = {Climate-driven distributional shifts have been well-documented for fisheries resources along the East Coast of the United States, yet little attention has been given to adjacent estuarine systems. The Chesapeake Bay is the largest estuary in the continental United States and serves as important habitat for a diversity of fishes and invertebrates, many of which are seasonal residents. Survey data indicate that relative abundance of finfish in Chesapeake Bay has diminished substantially, while coastwide stock status has remained unchanged. In response to warming, seasonal estuarine residents may remain in coastal waters or inhabit a northerly estuary, but the extent to which changing environmental conditions may drive exchange between the coastal ocean and estuarine systems remains unresolved. This study analyzed data collected from 2008 to 2019 by three fisheries-independent trawl surveys to explore temporal patterns and associated environmental drivers of the estuarine–coastal ocean exchange in the Mid-Atlantic for eight economically and ecologically important species. Relative habitat utilization of Chesapeake Bay declined for most species, while utilization patterns for Delaware Bay were largely constant or increasing over time. Broad-scale, multispecies analyses of relative habitat utilization time series revealed that the North Atlantic Oscillation ({NAO}) was an important driver of Chesapeake Bay exchange, but that average Apr/May coastal ocean bottom temperature was significant for Delaware Bay. Collectively, the results demonstrate that several Mid-Atlantic species have altered their estuarine habitat use over time, climate drivers associated with estuarine–coastal ocean exchange operate on different time scales, and that the impacts of warming within the Mid-Atlantic vary spatially.},
pages = {615--628},
number = {6},
journaltitle = {Fisheries Oceanography},
author = {Schonfeld, Adena J. and Gartland, James and Latour, Robert J.},
urldate = {2022-11-02},
date = {2022},
langid = {english},
note = {\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1111/fog.12611},
keywords = {climate change, Chesapeake Bay, dynamic factor analysis, ecosystem exchange, quantitative fisheries ecology},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\GSNGARVS\\Schonfeld et al. - 2022 - Spatial differences in estuarine utilization by se.pdf:application/pdf;Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\8L95MKRE\\Schonfeld et al. - 2022 - Spatial differences in estuarine utilization by se.pdf:application/pdf;Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\22R23CIQ\\Schonfeld et al. - 2022 - Spatial differences in estuarine utilization by se.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\B7GJJU76\\fog.html:text/html},
}
@article{depiper_learning_2021,
title = {Learning by doing: collaborative conceptual modelling as a path forward in ecosystem-based management},
volume = {78},
issn = {1054-3139},
url = {https://doi.org/10.1093/icesjms/fsab054},
doi = {10.1093/icesjms/fsab054},
shorttitle = {Learning by doing},
abstract = {Managers, stakeholders, and scientists recognize the need for collaborative, transparent, integrated approaches to complex resource management issues, and frameworks to address these complex issues are developing. Through the course of 2019, the Mid-Atlantic Fishery Management Council developed a conceptual model of ecosystem linkages and risks for summer flounder, a species of recreational and commercial fisheries importance. The proximal aim of the model was to develop a list of integrated management questions that could be refined and addressed through a future quantitative management strategy evaluation. As such, this conceptual model served as a scoping tool. However, the true value of the conceptual model lays elsewhere: familiarizing resource managers historically focused on single-species management with the potential utility of an ecosystem approach to management. This paper details the goals and development of the conceptual model and situates this process in the broader context of best practices for collaborative open science and scientific reproducibility. Further, it highlights a successful path by which the shift towards ecosystem-based management can be actuated.},
pages = {1217--1228},
number = {4},
journaltitle = {{ICES} Journal of Marine Science},
shortjournal = {{ICES} Journal of Marine Science},
author = {{DePiper}, Geret and Gaichas, Sarah and Muffley, Brandon and Ardini, Greg and Brust, Jeffrey and Coakley, Jessica and Dancy, Kiley and Elliott, G Warren and Leaning, Dustin C and Lipton, Douglas and {McNamee}, Jason and Perretti, Charles and Rootes-Murdy, Kirby and Wilberg, Michael J},
urldate = {2022-08-08},
date = {2021-08-04},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\C3RGFFYZ\\DePiper et al. - 2021 - Learning by doing collaborative conceptual modell.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\3MH8VAJU\\6207633.html:text/html},
}
@article{caracappa_northeast_2022,
title = {A northeast United States Atlantis marine ecosystem model with ocean reanalysis and ocean color forcing},
volume = {471},
issn = {0304-3800},
url = {https://www.sciencedirect.com/science/article/pii/S030438002200148X},
doi = {10.1016/j.ecolmodel.2022.110038},
abstract = {The northeast United States Atlantis model ({NEUSv}2) is an end-to-end ecosystem model that can simulate biogeochemical, ecological, fishery, management, and socio-economic processes within marine ecosystems. As a major update to the original model, {NEUSv}2 includes changes to the model's functional group definitions and forcing data. {NEUSv}2 is the first Atlantis model to use a satellite-ocean-color-derived phytoplankton size class model that was tuned specifically for the region to force marine primary production. Additionally, physical ocean variables (currents, temperature, and salinity) were updated using a high-resolution global ocean reanalysis. Despite its coarse resolution, {NEUSv}2 was capable of reproducing the broad spatial patterns seen in the physical and biological forcing sources, with the exception of some circulation features. {NEUSv}2 produced plausible zooplankton and planktivore biomass, a stable lower trophic food web, and recent trends in zooplankton biomass. {NEUSv}2 meets calibration criteria for the persistence and long-term stability of functional group biomass. Given the success of this new Atlantis forcing approach, we detail the observations and challenges regarding spatial scale-related processes, data assimilation, and biological calibration. We also discuss possible tradeoffs with model scope, calibration, and the availability of feedback mechanisms. This {NEUSv}2 hindcast is well suited for exploring ecosystem-level sensitivity to lower trophic processes and for testing alternative biogeochemical forcing. Further developments will improve model performance for higher trophic levels.},
pages = {110038},
journaltitle = {Ecological Modelling},
shortjournal = {Ecological Modelling},
author = {Caracappa, Joseph C. and Beet, Andrew and Gaichas, Sarah and Gamble, Robert J. and Hyde, Kimberly J. W. and Large, Scott I. and Morse, Ryan E. and Stock, Charles A. and Saba, Vincent S.},
urldate = {2022-08-08},
date = {2022-09-01},
langid = {english},
keywords = {Atlantis, biogeochemical forcing, end-to-end models, global reanalysis, lower trophic levels, marine ecosystem models, ocean color, primary production},
file = {ScienceDirect Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\DILX5W83\\Caracappa et al. - 2022 - A northeast United States Atlantis marine ecosyste.pdf:application/pdf;ScienceDirect Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\S672JAVG\\S030438002200148X.html:text/html},
}
@article{christiansen_emergence_2022,
title = {Emergence of Large-Scale Hydrodynamic Structures Due to Atmospheric Offshore Wind Farm Wakes},
volume = {9},
issn = {2296-7745},
url = {https://www.frontiersin.org/article/10.3389/fmars.2022.818501},
abstract = {The potential impact of offshore wind farms through decreasing sea surface wind speed on the shear forcing and its consequences for the ocean dynamics are investigated. Based on the unstructured-grid model {SCHISM}, we present a new cross-scale hydrodynamic model setup for the southern North Sea, which enables high-resolution analysis of offshore wind farms in the marine environment. We introduce an observational-based empirical approach to parameterize the atmospheric wakes in a hydrodynamic model and simulate the seasonal cycle of the summer stratification in consideration of the recent state of wind farm development in the southern North Sea. The simulations show the emergence of large-scale attenuation in the wind forcing and associated alterations in the local hydro- and thermodynamics. The wake effects lead to unanticipated spatial variability in the mean horizontal currents and to the formation of large-scale dipoles in the sea surface elevation. Induced changes in the vertical and lateral flow are sufficiently strong to influence the residual currents and entail alterations of the temperature and salinity distribution in areas of wind farm operation. Ultimately, the dipole-related processes affect the stratification development in the southern North Sea and indicate potential impact on marine ecosystem processes. In the German Bight, in particular, we observe large-scale structural change in stratification strength, which eventually enhances the stratification during the decline of the summer stratification toward autumn.},
journaltitle = {Frontiers in Marine Science},
author = {Christiansen, Nils and Daewel, Ute and Djath, Bughsin and Schrum, Corinna},
urldate = {2022-03-09},
date = {2022},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\TEC2AI85\\Christiansen et al. - 2022 - Emergence of Large-Scale Hydrodynamic Structures D.pdf:application/pdf},
}
@article{quintana-rizzo_residency_2021,
title = {Residency, demographics, and movement patterns of North Atlantic right whales Eubalaena glacialis in an offshore wind energy development area in southern New England, {USA}},
volume = {45},
issn = {1863-5407, 1613-4796},
url = {https://www.int-res.com/abstracts/esr/v45/p251-268/},
doi = {10.3354/esr01137},
abstract = {Offshore wind energy development is growing quickly around the world. In southern New England, {USA}, one of the largest commercial offshore wind energy farms in the {USA} will be established in the waters off Massachusetts and Rhode Island, an area used by the Critically Endangered North Atlantic right whale Eubalaena glacialis. Prior to 2011, little was known about the use of this area by right whales. We examined aerial survey data collected between 2011-2015 and 2017-2019 to quantify right whale distribution, residency, demography, and movements in the region. Right whale occurrence increased during the study period. Since 2017, whales have been sighted in the area nearly every month, with peak sighting rates between late winter and spring. Model outputs suggest that 23\% of the species’ population is present from December through May, and the mean residence time has tripled to an average of 13 d during these months. Age and sex ratios of the individuals present in the area are similar to those of the species as a whole, with adult males the most common demographic group. Movement models showed that southern New England is an important destination for right whales, including conceptive and reproductive females, and qualitative observations included animals feeding and socializing. Implementing mitigation procedures in coordination with these findings will be crucial in lessening the potential impacts on right whales from construction noise, increased vessel traffic, and habitat disruption in this region.},
pages = {251--268},
journaltitle = {Endangered Species Research},
author = {Quintana-Rizzo, E. and Leiter, S. and Cole, T. V. N. and Hagbloom, M. N. and Knowlton, A. R. and Nagelkirk, P. and OBrien, O. and Khan, C. B. and Henry, A. G. and Duley, P. A. and Crowe, L. M. and Mayo, C. A. and Kraus, S. D.},
urldate = {2022-03-09},
date = {2021-07-29},
langid = {english},
keywords = {Aerial surveys, Alternative energy, Migratory species},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\LJSI7QIZ\\Quintana-Rizzo et al. - 2021 - Residency, demographics, and movement patterns of .pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\E7DCYRH5\\p251-268.html:text/html},
}
@article{du_pontavice_incorporating_nodate,
title = {Incorporating environmental effects from ocean models improves a marine fish stock assessment},
journaltitle = {{ICES} Journal of Marine Science},
author = {du Pontavice, H. and Miller, Timothy J. and Stock, Brian C. and Chen, Zhuomin and Saba, Vincent S.},
}
@article{gawarkiewicz_increasing_nodate,
title = {Increasing Frequency of Mid-depth Salinity Maximum Intrusions in the Middle Atlantic Bight},
journaltitle = {Journal of Geophysical Research: Oceans},
author = {Gawarkiewicz, Glen and Fratantoni, Paula and Bahr, Frank and Ellertson, Aubrey},
}
@article{farr_assessment_2021,
title = {An assessment of marine, estuarine, and riverine habitat vulnerability to climate change in the Northeast U.S.},
volume = {16},
issn = {1932-6203},
url = {https://journals.plos.org/plosone/article?id=10.1371/journal.pone.0260654},
doi = {10.1371/journal.pone.0260654},
abstract = {Climate change is impacting the function and distribution of habitats used by marine, coastal, and diadromous species. These impacts often exacerbate the anthropogenic stressors that habitats face, particularly in the coastal environment. We conducted a climate vulnerability assessment of 52 marine, estuarine, and riverine habitats in the Northeast U.S. to develop an ecosystem-scale understanding of the impact of climate change on these habitats. The trait-based assessment considers the overall vulnerability of a habitat to climate change to be a function of two main components, sensitivity and exposure, and relies on a process of expert elicitation. The climate vulnerability ranks ranged from low to very high, with living habitats identified as the most vulnerable. Over half of the habitats examined in this study are expected to be impacted negatively by climate change, while four habitats are expected to have positive effects. Coastal habitats were also identified as highly vulnerable, in part due to the influence of non-climate anthropogenic stressors. The results of this assessment provide regional managers and scientists with a tool to inform habitat conservation, restoration, and research priorities, fisheries and protected species management, and coastal and ocean planning.},
pages = {e0260654},
number = {12},
journaltitle = {{PLOS} {ONE}},
shortjournal = {{PLOS} {ONE}},
author = {Farr, Emily R. and Johnson, Michael R. and Nelson, Mark W. and Hare, Jonathan A. and Morrison, Wendy E. and Lettrich, Matthew D. and Vogt, Bruce and Meaney, Christopher and Howson, Ursula A. and Auster, Peter J. and Borsuk, Frank A. and Brady, Damian C. and Cashman, Matthew J. and Colarusso, Phil and Grabowski, Jonathan H. and Hawkes, James P. and Mercaldo-Allen, Renee and Packer, David B. and Stevenson, David K.},
urldate = {2022-03-02},
date = {2021-12-09},
langid = {english},
note = {Publisher: Public Library of Science},
keywords = {Climate change, Anthropogenic climate change, Habitats, Marine fish, Reefs, Surface water, Water columns, Wetlands},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\6RBHCZHP\\Farr et al. - 2021 - An assessment of marine, estuarine, and riverine h.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\XIDW7DS9\\article.html:text/html},
}
@article{schick_striking_2009,
title = {Striking the right balance in right whale conservation},
volume = {66},
issn = {0706-652X},
url = {https://cdnsciencepub.com/doi/10.1139/F09-115},
doi = {10.1139/F09-115},
pages = {1399--1403},
number = {9},
journaltitle = {Canadian Journal of Fisheries and Aquatic Sciences},
shortjournal = {Can. J. Fish. Aquat. Sci.},
author = {Schick, Robert S. and Halpin, Patrick N. and Read, Andrew J. and Slay, Christopher K. and Kraus, Scott D. and Mate, Bruce R. and Baumgartner, Mark F. and Roberts, Jason J. and Best, Benjamin D. and Good, Caroline P. and Loarie, Scott R. and Clark, James S.},
urldate = {2022-03-09},
date = {2009-09},
note = {Publisher: {NRC} Research Press},
file = {Submitted Version:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\HND4AUNI\\Schick et al. - 2009 - Striking the right balance in right whale conserva.pdf:application/pdf},
}
@book{boem_vineyard_2020,
title = {Vineyard Wind 1 Offshore Wind Energy Project Supplement to the Draft Environmental Impact Statement. {OCS} {EIS}/{EA}, {BOEM} 2020-025},
url = {https://www.boem.gov/sites/default/files/documents/renewable-energy/Vineyard-Wind-1-Supplement-to-EIS.pdf},
pagetotal = {420},
author = {{BOEM}},
urldate = {2022-02-11},
date = {2020},
file = {Vineyard-Wind-1-Supplement-to-EIS.pdf:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\YKRBWL2B\\Vineyard-Wind-1-Supplement-to-EIS.pdf:application/pdf},
}
@article{perretti_regime_2017,
title = {Regime shifts in fish recruitment on the Northeast {US} Continental Shelf},
volume = {574},
issn = {0171-8630, 1616-1599},
url = {http://www.int-res.com/abstracts/meps/v574/p1-11/},
doi = {10.3354/meps12183},
abstract = {There is accumulating evidence for decadal-scale regime shifts at the base of the food web on the Northeast {US} Continental Shelf. However, less evidence exists for regime shifts in fish recruitment success, particularly for synchronized regimes across multiple species. Here, we analyzed stock assessment output and survey data to test for regimes in the recruitment success of 18 commercially important marine species over a 29 yr timespan. We then tested whether recruitment regimes coincide with regimes in the zooplankton community, and whether the abundance of large spawners could explain the patterns in recruitment. We found evidence for 3 decadal-scale recruitment regimes: low recruitment success in the 1980s, high success in the 1990s, and a return to low recruitment success in the 2000s. This general pattern was found in all datasets of recruitment. The abundance of large spawners did not appear to be a broad-scale driver of recruitment success; however, recruitment regimes coincided with regimes in copepod abundance and size structure.},
pages = {1--11},
journaltitle = {Marine Ecology Progress Series},
shortjournal = {Mar. Ecol. Prog. Ser.},
author = {Perretti, Ct and Fogarty, Mj and Friedland, Kd and Hare, Ja and Lucey, Sm and {McBride}, Rs and Miller, Tj and Morse, Re and O’Brien, L and Pereira, Jj and Smith, La and Wuenschel, Mj},
urldate = {2022-02-10},
date = {2017-07-04},
langid = {english},
file = {Perretti et al. - 2017 - Regime shifts in fish recruitment on the Northeast.pdf:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\NRAGBLGA\\Perretti et al. - 2017 - Regime shifts in fish recruitment on the Northeast.pdf:application/pdf;Perretti et al. - 2017 - Regime shifts in fish recruitment on the Northeast.pdf:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\ZXKKMXZZ\\Perretti et al. - 2017 - Regime shifts in fish recruitment on the Northeast.pdf:application/pdf},
}
@article{johnson_savory_2015,
title = {The Savory Swimmer Swims North: A Northern Range Extension of the Blue Crab Callinectes Sapidus?},
volume = {35},
issn = {0278-0372},
url = {https://doi.org/10.1163/1937240X-00002293},
doi = {10.1163/1937240X-00002293},
shorttitle = {The Savory Swimmer Swims North},
abstract = {Worldwide, climate-change is shifting species distributions poleward. Here I present recent (2012-2014) observations of the blue crab, Callinectes {sapidusRathbun}, 1896, in the Gulf of Maine ({GoM}), north of its historical range of Cape Cod, Massachusetts. To test the hypothesis of a climate-driven range expansion, I examined near-surface ocean temperatures. On average, ocean temperatures in the {GoM} in summer 2012 and 2013 were up to \$1.3{\textasciicircum}{\textbackslash}circ\{{\textbackslash}rm\{C\}\}\$ higher than the average of the previous decade, suggesting that warmer waters may have promoted the recruitment of C. sapidus to the {GoM}. Previous ephemeral populations of C. sapidus in the Gulf of Maine have been reported since the 1860s. Recent observations and continued warming in the northwest Atlantic may signal a permanent poleward expansion of C. sapidus into the {GoM}. If so, then a key goal for ecologists and managers will be to understand the effect of C. sapidus on {GoM} food-webs and fisheries.},
pages = {105--110},
number = {1},
journaltitle = {Journal of Crustacean Biology},
shortjournal = {Journal of Crustacean Biology},
author = {Johnson, David Samuel},
urldate = {2022-02-10},
date = {2015-01-01},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\XHPF9TU5\\Johnson - 2015 - The Savory Swimmer Swims North A Northern Range E.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\6A9YDFM4\\2547817.html:text/html},
}
@article{deibel_predictability_2009,
title = {Predictability of patches of neritic salps and doliolids (Tunicata, Thaliacea)},
volume = {31},
issn = {0142-7873, 1464-3774},
url = {https://academic.oup.com/plankt/article-lookup/doi/10.1093/plankt/fbp091},
doi = {10.1093/plankt/fbp091},
pages = {1571--1579},
number = {12},
journaltitle = {Journal of Plankton Research},
shortjournal = {Journal of Plankton Research},
author = {Deibel, D. and Paffenhofer, G.-A.},
urldate = {2022-02-10},
date = {2009-12-01},
langid = {english},
file = {Deibel and Paffenhofer - 2009 - Predictability of patches of neritic salps and dol.pdf:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\5DQSAXWX\\Deibel and Paffenhofer - 2009 - Predictability of patches of neritic salps and dol.pdf:application/pdf},
}
@article{powell_ocean_2020,
title = {Ocean quahogs (Arctica islandica) and Atlantic surfclams (Spisula solidissima) on the Mid-Atlantic Bight continental shelf and Georges Bank: The death assemblage as a recorder of climate change and the reorganization of the continental shelf benthos},
volume = {537},
issn = {0031-0182},
url = {https://www.sciencedirect.com/science/article/pii/S0031018218309118},
doi = {10.1016/j.palaeo.2019.05.027},
shorttitle = {Ocean quahogs (Arctica islandica) and Atlantic surfclams (Spisula solidissima) on the Mid-Atlantic Bight continental shelf and Georges Bank},
abstract = {The degree to which evidence of range shifts in shelf biomass dominants, Atlantic surfclams and ocean quahogs, as a function of climate change is examined by comparing the dissimilarity in distribution of the living community and the record of habitation ensconced in the death assemblage. Comparison of the distribution of live animals and dead shells reveals for both species that live animals are rarely found where dead shells were not collected, but dead shells were collected at a substantively larger number of sites than where live animals were found. The geographic footprint resolved by the dead shells was much broader than that of live animals. Extensive spatially-coherent regions exist inshore and offshore of the present-day habitat of occupation where evidence of previous occupation exists. Sites where ocean quahog shells were found without live ocean quahogs included a portion of the continental shelf inshore of the present-day habitable range, an area only habitable under colder climatic conditions than observed today. Surfclam shells were found offshore of the present-day habitable region, in deeper water: additional warming of bottom waters offshore would be necessary for surfclams to occupy the region now occupied solely by dead shells. The death assemblage shows that these biomass dominants have repositioned themselves across the continental shelf during the past and this repositioning certainly is driven by changes in bottom water temperature. Moreover, the distribution of surfclam shells indicates that the death assemblage may provide a possible window into the future, as movement of the present-day population is towards these deeper-water previously-occupied regions. Overall, the death assemblage may provide an important source of information on range shifts sparing the need to carry out extensive and frequent benthic surveys and may permit reconstruction of ongoing shifts in community composition as a product of climate change when adequate survey data are not available.},
pages = {109205},
journaltitle = {Palaeogeography, Palaeoclimatology, Palaeoecology},
shortjournal = {Palaeogeography, Palaeoclimatology, Palaeoecology},
author = {Powell, Eric N. and Ewing, Anja M. and Kuykendall, Kelsey M.},
urldate = {2022-02-10},
date = {2020-01-01},
langid = {english},
keywords = {Conservation paleobiology, Geographic distribution, Live-dead comparison, Range shift, Spatial time averaging, Species interaction},
file = {ScienceDirect Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\FVKEAPR5\\S0031018218309118.html:text/html},
}
@article{pace_two-hundred_2018,
title = {Two-hundred year record of increasing growth rates for ocean quahogs (Arctica islandica) from the northwestern Atlantic Ocean},
volume = {503},
issn = {0022-0981},
url = {https://www.sciencedirect.com/science/article/pii/S0022098117303568},
doi = {10.1016/j.jembe.2018.01.010},
abstract = {Ocean quahogs [Arctica islandica (Linnaeus, 1769)] are the longest-lived, non-colonial animal known today, with a maximum life span exceeding 500 years. Ocean quahogs are a commercially important bivalve, inhabiting the continental shelf of the North Atlantic basin. We examined growth rates of ocean quahogs that were fully recruited to the commercial fishery ({\textgreater}80-mm shell length) from four sites covering the range of the stock along the east coast of the U.S. through analysis of annual growth lines in the hinge plate. Both geographic and temporal differences (on a scale of decadal or longer) in growth rates exist throughout the range of the stock. The age at which animals reached 60, 80, and 90 mm decreased significantly, and average growth rates to 60, 80, and 90 mm increased significantly with birth year at a New Jersey and a Long Island site, both located in the southwestern portion of the stock, since the late 1700s/early 1800s, likely in response to increasing bottom water temperatures. That is, growth rates vary temporally with birth date at the southwestern sites, with younger animals growing at a much faster rate in recent decades than those born many decades previously, whereas at the northern sites off southern New England and on Georges Bank, changes in growth rates through time are limited to older adult animals or absent altogether. Thus, at the southern portion of the range, variation in growth rate over time exists in all phases of ocean quahog life, whereas on Georges Bank, little evidence exists for any differential in growth rate over the last {\textasciitilde}200 years. The fact that ocean quahogs record the rise in ocean temperatures after the Little Ice Age in the Mid-Atlantic Bight southeast of southern New England, yet demonstrate little evidence of such a rise in the southern New England and Georges Bank region, would suggest a differential response of ocean circulation and its control of bottom water temperature between the northern and southern portions of the Mid-Atlantic Bight over the last 200+ years.},
pages = {8--22},
journaltitle = {Journal of Experimental Marine Biology and Ecology},
shortjournal = {Journal of Experimental Marine Biology and Ecology},
author = {Pace, Sara M. and Powell, Eric N. and Mann, Roger},
urldate = {2022-02-10},
date = {2018-06-01},
langid = {english},
keywords = {Climate change, Growth, Little Ice Age, Ocean quahog},
file = {ScienceDirect Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\IKCT8QWJ\\S0022098117303568.html:text/html},
}
@article{worm_predator_2003,
title = {Predator diversity hotspots in the blue ocean},
volume = {100},
rights = {Copyright © 2003, The National Academy of Sciences},
issn = {0027-8424, 1091-6490},
url = {https://www.pnas.org/content/100/17/9884},
doi = {10.1073/pnas.1333941100},
abstract = {Concentrations of biodiversity, or hotspots, represent conservation priorities in terrestrial ecosystems but remain largely unexplored in marine habitats. In the open ocean, many large predators such as tunas, sharks, billfishes, and sea turtles are of current conservation concern because of their vulnerability to overfishing and ecosystem role. Here we use scientific-observer records from pelagic longline fisheries in the Atlantic and Pacific Oceans to show that oceanic predators concentrate in distinct diversity hotspots. Predator diversity consistently peaks at intermediate latitudes (20–30° N and S), where tropical and temperate species ranges overlap. Individual hotspots are found close to prominent habitat features such as reefs, shelf breaks, or seamounts and often coincide with zooplankton and coral reef hotspots. Closed-area models in the northwest Atlantic predict that protection of hotspots outperforms other area closures in safeguarding threatened pelagic predators from ecological extinction. We conclude that the seemingly monotonous landscape of the open ocean shows rich structure in species diversity and that these features should be used to focus future conservation efforts.},
pages = {9884--9888},
number = {17},
journaltitle = {Proceedings of the National Academy of Sciences},
shortjournal = {{PNAS}},
author = {Worm, Boris and Lotze, Heike K. and Myers, Ransom A.},
urldate = {2022-02-10},
date = {2003-08-19},
langid = {english},
pmid = {12907699},
note = {Publisher: National Academy of Sciences
Section: Biological Sciences},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\RYABUMGF\\Worm et al. - 2003 - Predator diversity hotspots in the blue ocean.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\UM6QF23W\\9884.html:text/html},
}
@article{madin_periodic_2006,
title = {Periodic swarms of the salp Salpa aspera in the Slope Water off the {NE} United States: Biovolume, vertical migration, grazing, and vertical flux},
volume = {53},
issn = {0967-0637},
url = {https://www.sciencedirect.com/science/article/pii/S0967063706000173},
doi = {10.1016/j.dsr.2005.12.018},
shorttitle = {Periodic swarms of the salp Salpa aspera in the Slope Water off the {NE} United States},
abstract = {Sampling during four summers over a twenty-seven year period has documented dense populations of Salpa aspera in the Slope Water south of New England, northeastern United States. The salps demonstrated a strong pattern of diel vertical migration, moving to depth (mostly 600–800m) during the day and aggregating in the epipelagic ({\textless}100m) at night. Filtration rates determined from both gut pigment analysis and direct feeding experiments indicated that both the aggregate and solitary stages filtered water at rates ranging from 0.5 to 6lh-1ml-1 biovolume. Maximum displacement volumes of salps measured were 5.7lm-2 in 1986 and 1.6lm-2 in 1993. Depending on the year, the sampled salp populations were calculated to clear between 8 and 74\% of the upper 50m during each 8h night. Total fecal output for the same populations was estimated to be between 5 and 91mgCm-2night-1. These results, and other observations, suggest this region is a salp “hot spot”, with swarms of S. aspera developing seasonally on a frequent basis.},
pages = {804--819},
number = {5},
journaltitle = {Deep Sea Research Part I: Oceanographic Research Papers},
shortjournal = {Deep Sea Research Part I: Oceanographic Research Papers},
author = {Madin, L. P. and Kremer, P. and Wiebe, P. H. and Purcell, J. E. and Horgan, E. H. and Nemazie, D. A.},
urldate = {2022-02-10},
date = {2006-05-01},
langid = {english},
keywords = {Atlantic Slope Water, Grazing, Salps, Vertical flux, Vertical migration, Zooplankton},
file = {ScienceDirect Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\76VQA2RT\\S0967063706000173.html:text/html},
}
@article{potter_horizontal_2011,
title = {Horizontal movement of ocean sunfish, Mola mola, in the northwest Atlantic},
volume = {158},
issn = {1432-1793},
url = {https://doi.org/10.1007/s00227-010-1578-2},
doi = {10.1007/s00227-010-1578-2},
abstract = {Data were retrieved from 25 ocean sunfish (Mola mola) that were tagged with pop-up satellite archival tags in the southern Gulf of Maine (n = 6), off Nantucket Island (n = 17), and off the coast of Georgia (n = 2) between September 2005 and March 2008. Tags remained attached from 7 to 242 days, with a mean attachment period of (X ± {SD}) 107.2 ± 80.6 days. Ocean sunfish tagged in the Gulf of Maine and southern New England left those areas in the late summer and early autumn and moved south along the continental shelf break. Fish traveled as far south as the Bahamas and the Gulf of Mexico. By moving south, sunfish experienced similar mean sea surface temperatures throughout the tagging period. The maximum straight-line distance traveled by a tagged Mola mola was 2,520 km in 130 days. Two tagged ocean sunfish entered the Gulf of Mexico, one in the December and one in July. Movements were associated with frontal features created by the Gulf Stream and fish moved farther offshore in 2007 when the Gulf Stream was deflected from the shelf break.},
pages = {531--540},
number = {3},
journaltitle = {Marine Biology},
shortjournal = {Mar Biol},
author = {Potter, Inga F. and Galuardi, Benjamin and Howell, W. Huntting},
urldate = {2022-02-10},
date = {2011-03-01},
langid = {english},
file = {Springer Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\YUG6HGHA\\Potter et al. - 2011 - Horizontal movement of ocean sunfish, Mola mola, i.pdf:application/pdf},
}
@article{caesar_current_2021,
title = {Current Atlantic Meridional Overturning Circulation weakest in last millennium},
volume = {14},
rights = {2021 The Author(s), under exclusive licence to Springer Nature Limited},
issn = {1752-0908},
url = {https://www.nature.com/articles/s41561-021-00699-z},
doi = {10.1038/s41561-021-00699-z},
abstract = {The Atlantic Meridional Overturning Circulation ({AMOC})—one of Earth’s major ocean circulation systems—redistributes heat on our planet and has a major impact on climate. Here, we compare a variety of published proxy records to reconstruct the evolution of the {AMOC} since about ad 400. A fairly consistent picture of the {AMOC} emerges: after a long and relatively stable period, there was an initial weakening starting in the nineteenth century, followed by a second, more rapid, decline in the mid-twentieth century, leading to the weakest state of the {AMOC} occurring in recent decades.},
pages = {118--120},
number = {3},
journaltitle = {Nature Geoscience},
shortjournal = {Nat. Geosci.},
author = {Caesar, L. and {McCarthy}, G. D. and Thornalley, D. J. R. and Cahill, N. and Rahmstorf, S.},
urldate = {2022-02-10},
date = {2021-03},
langid = {english},
note = {Number: 3
Publisher: Nature Publishing Group},
keywords = {Climate change, Physical oceanography, Palaeoclimate},
file = {Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\DPJZKDCQ\\s41561-021-00699-z.html:text/html;Submitted Version:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\NNTXSEI2\\Caesar et al. - 2021 - Current Atlantic Meridional Overturning Circulatio.pdf:application/pdf},
}
@article{caesar_observed_2018,
title = {Observed fingerprint of a weakening Atlantic Ocean overturning circulation},
volume = {556},
rights = {2018 Macmillan Publishers Ltd., part of Springer Nature},
issn = {1476-4687},
url = {https://www.nature.com/articles/s41586-018-0006-5},
doi = {10.1038/s41586-018-0006-5},
abstract = {The Atlantic meridional overturning circulation ({AMOC})—a system of ocean currents in the North Atlantic—has a major impact on climate, yet its evolution during the industrial era is poorly known owing to a lack of direct current measurements. Here we provide evidence for a weakening of the {AMOC} by about 3 ± 1 sverdrups (around 15 per cent) since the mid-twentieth century. This weakening is revealed by a characteristic spatial and seasonal sea-surface temperature ‘fingerprint’—consisting of a pattern of cooling in the subpolar Atlantic Ocean and warming in the Gulf Stream region—and is calibrated through an ensemble of model simulations from the {CMIP}5 project. We find this fingerprint both in a high-resolution climate model in response to increasing atmospheric carbon dioxide concentrations, and in the temperature trends observed since the late nineteenth century. The pattern can be explained by a slowdown in the {AMOC} and reduced northward heat transport, as well as an associated northward shift of the Gulf Stream. Comparisons with recent direct measurements from the {RAPID} project and several other studies provide a consistent depiction of record-low {AMOC} values in recent years.},
pages = {191--196},
number = {7700},
journaltitle = {Nature},
author = {Caesar, L. and Rahmstorf, S. and Robinson, A. and Feulner, G. and Saba, V.},
urldate = {2022-02-10},
date = {2018-04},
langid = {english},
note = {Number: 7700
Publisher: Nature Publishing Group},
keywords = {Physical oceanography, Climate and Earth system modelling, Ocean sciences},
file = {Accepted Version:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\UEBMA38Z\\Caesar et al. - 2018 - Observed fingerprint of a weakening Atlantic Ocean.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\STMDY3GI\\s41586-018-0006-5.html:text/html},
}
@article{miles_offshore_2021,
title = {Offshore Wind Energy and the Mid-Atlantic Cold Pool: A Review of Potential Interactions},
volume = {55},
doi = {10.4031/MTSJ.55.4.8},
shorttitle = {Offshore Wind Energy and the Mid-Atlantic Cold Pool},
abstract = {Abstract
The U.S. East Coast has 1.7 million acres of federal bottom under lease for the development of wind energy installations, with plans for more than 1,500 foundations to be placed. The scale of these wind farms has the potential to alter the unique and delicate oceanographic
conditions along the expansive Atlantic continental shelf, a region characterized by a strong seasonal thermocline that overlies cold bottom water, known as the “Cold Pool.” Strong seasonal stratification traps cold (typically less than 10°C) water above the ocean bottom sustaining
a boreal fauna that represents vast fisheries, including the most lucrative shellfish fisheries in the United States. This paper reviews the existing literature and research pertaining to the ways in which offshore wind farms may alter processes that establish, maintain, and degrade stratification
associated with the Cold Pool through vertical mixing in this seasonally dynamic system. Changes in stratification could have important consequences in Cold Pool setup and degradation, processes fundamental to high fishery productivity of the region. The potential for these multiple wind energy
arrays to alter oceanographic processes and the biological systems that rely on them is possible; however, a great deal of uncertainty remains about the nature and scale of these interactions. Research should be prioritized that identifies stratification thresholds of influence, below which
turbines and wind farm arrays may alter oceanographic processes. These should be examined within context of spatial and seasonal dynamics of the Cold Pool and offshore wind lease areas to identify potential areas of further study.},
pages = {72--87},
number = {4},
journaltitle = {Marine Technology Society Journal},
shortjournal = {Marine Technology Society Journal},
author = {Miles, Travis and Murphy, Sarah and Kohut, Josh and Borsetti, Sarah and Munroe, Daphne},
date = {2021-07-01},
keywords = {Mid-Atlantic Cold Pool, ocean interactions, offshore wind},
}
@article{gawarkiewicz_characteristics_2019,
title = {Characteristics of an Advective Marine Heatwave in the Middle Atlantic Bight in Early 2017},
volume = {6},
issn = {2296-7745},
url = {https://www.frontiersin.org/article/10.3389/fmars.2019.00712},
abstract = {There has been wide interest in Marine Heatwaves and their ecological consequences in recent years. Most analyses have focused on remotely sensed sea surface temperature data due to the temporal and spatial coverage it provides in order to establish the presence and duration of Heatwaves. Using hydrographic data from a variety of sources, we show that an advective Marine Heatwave was initiated by an event in late December of 2016 south of New England, with temperature anomalies measuring up to 6°C and salinity anomalies exceeding 1 {PSU}. Similar features were observed off of New Jersey in February 2017, and are associated with the Shelfbreak Front migrating from its normal position to mid-shelf or further onshore. Shelf water of 34 {PSU} was observed just north of Cape Hatteras at the 30 m isobath and across the continental shelf in late April 2017. These observations reveal that the 2017 Marine Heatwave was associated with a strong positive salinity anomaly, that its total duration was approximately 4 months, and its advective path extended roughly 850 km along the length of the continental shelf in the Middle Atlantic Bight. The southward advective velocity implied by the arrival north of Cape Hatteras is consistent with previous estimates of alongshelf velocity for the region. The origin of this Marine Heatwave is likely related to cross-shelf advection driven by the presence of a Warm Core Ring adjacent to the shelfbreak south of New England.},
journaltitle = {Frontiers in Marine Science},
author = {Gawarkiewicz, Glen and Chen, Ke and Forsyth, Jacob and Bahr, Frank and Mercer, Anna M. and Ellertson, Aubrey and Fratantoni, Paula and Seim, Harvey and Haines, Sara and Han, Lu},
urldate = {2022-02-10},
date = {2019},
file = {Full Text PDF:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\9VF6DG7F\\Gawarkiewicz et al. - 2019 - Characteristics of an Advective Marine Heatwave in.pdf:application/pdf},
}
@article{chen_mesoscale_2022,
title = {Mesoscale and Submesoscale Shelf-Ocean Exchanges Initialize an Advective Marine Heatwave},
volume = {127},
url = {https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2021JC017927},
doi = {https://doi.org/10.1029/2021JC017927},
abstract = {Abstract Observations and high-resolution numerical modeling are used to investigate the dynamical processes related to the initiation of an advective Marine Heatwave in the Middle Atlantic Bight of the Northwest Atlantic continental shelf. Both the observations and the model identify two significant cross-shelf intrusions in November 2016 and January 2017, with the latter inducing large-magnitude water mass anomalies across the shelf. Model prognostic fields reveal the importance of the combination of cyclonic eddies or ringlets and upwelling-favorable winds in producing the large-distance cross-shelf penetration and temperature/salinity anomalies. The cyclonic eddies in close proximity to the shelfbreak set up local along-isobath pressure gradients and provide favorable conditions for the intensification of the shelfbreak front, both processes driving cross-isobath intrusions of warm, salty offshore water onto the outer continental shelf. Subsequently, strong and persistent upwelling-favorable winds drive a rapid, bottom intensified cross-shelf penetration in January 2017 composed of the anomalous water mass off the shelfbreak. The along-shelf settings including realistic representation of bathymetric features are essential in the characteristics of the cross-shelf penetration. The results highlight the importance of smaller scale cyclonic eddies and the intricacy of the interplay between multiple processes to drive significant cross-shelf events.},
pages = {e2021JC017927},
number = {1},
journaltitle = {Journal of Geophysical Research: Oceans},
author = {Chen, Ke and Gawarkiewicz, Glen and Yang, Jiayan},
date = {2022},
note = {\_eprint: https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2021JC017927},
keywords = {cross-shelf exchange, drivers of Marine heatwave, pressure gradient setup, shelfbreak front and frontogenesis, warm core rings and cyclonic eddies, wind-driven upwelling and bottom intrusion},
}
@article{friedland_middle_2022,
title = {The Middle Atlantic Bight Cold Pool is warming and shrinking: Indices from in situ autumn seafloor temperatures},
volume = {31},
issn = {1365-2419},
url = {https://onlinelibrary.wiley.com/doi/abs/10.1111/fog.12573},
doi = {10.1111/fog.12573},
shorttitle = {The Middle Atlantic Bight Cold Pool is warming and shrinking},
abstract = {The Cold Pool feature of the Middle Atlantic Bight ({MAB}) is a body of cold bottom water that develops in the spring and persists through the summer-autumn months. It is maintained by northerly currents and can be traced back to Arctic water masses. The Cold Pool provides habitat for many boreal species at latitudes far south of their normal range and plays an important role in the population dynamics of lower and upper trophic level organisms. Here, we describe changes in the extent and thermal properties of the Cold Pool using both observations and models. Two indices are developed based on a gridded, interpolated bottom temperature dataset; the first is a mean temperature indicator, and the second is a spatial extent indicator. The temperature indicator showed a significant increasing trend over the study period 1968–2019 and a single change point in 2008. Similarly, the area indicator declined significantly, also displaying a change point in 2008. Cold Pool maximum temperature and minimum size were observed in 2017, which is also known as a heatwave year in the {MAB}. The indices presented here support the view of a rapidly warming Cold Pool that is being limited in its spatial extent. Changes in Cold Pool hydrography will likely affect boreal species distributions and total ecosystem productivity.},
pages = {217--223},
number = {2},
journaltitle = {Fisheries Oceanography},
author = {Friedland, Kevin D. and Miles, Travis and Goode, Andrew G. and Powell, Eric N. and Brady, Damian C.},
urldate = {2022-02-10},
date = {2022},
langid = {english},
note = {\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1111/fog.12573},
keywords = {climate change, Cold Pool, ecosystem, regime shift, temperature},
file = {Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\JG9MK62Q\\fog.html:text/html},
}
@article{gangopadhyay_census_2020,
title = {A Census of the Warm-Core Rings of the Gulf Stream: 1980–2017},
volume = {125},
issn = {2169-9291},
url = {https://onlinelibrary.wiley.com/doi/abs/10.1029/2019JC016033},
doi = {10.1029/2019JC016033},
shorttitle = {A Census of the Warm-Core Rings of the Gulf Stream},
abstract = {A census of Gulf Stream ({GS}) warm-core rings ({WCRs}) is presented based on 38 years (1980–2017) of data. The census documents formation and demise times and locations, and formation size for all 961 {WCRs} formed in the study period that live for a week or more. A clear regime shift was observed around the Year 2000 and was reported by a subset of authors (Gangopadhyay et al., 2019, https://doi.org/10.1038/s41598-019-48661-9). The {WCR} formation over the whole region (75–55°W) increased from an average of 18 per year during Regime 1 (1980–1999) to 33 per year during Regime 2 (2000–2017). For geographic analysis formation locations were grouped in four 5° zones between 75°W and 55°W. Seasonally, {WCR} formations show a significant summer maxima and winter minima, a pattern that is consistent through all zones and both temporal regimes. The lifespan and size distribution show progressively more rings with higher longevity and greater size when formed to the east of 70°W. The average lifespan of the {WCRs} in all four zones decreased by 20–40\% depending on zones and/or seasons from Regime 1 to Regime 2, while the size distribution remained unchanged across regimes. The ring footprint index, a first-order signature of impact of the {WCRs} on the slope, increased significantly (26–90\%) for all zones from Regime 1 to Regime 2, with the highest percent increase in Zone 2 (70–65°W). This observational study establishes critical statistical and dynamical benchmarks for validating numerical models and highlights the need for further dynamical understanding of the {GS}-ring formation processes.},
pages = {e2019JC016033},
number = {8},
journaltitle = {Journal of Geophysical Research: Oceans},
author = {Gangopadhyay, Avijit and Gawarkiewicz, Glen and Silva, E. Nishchitha S. and Silver, Adrienne M. and Monim, M. and Clark, Jenifer},
urldate = {2022-02-10},
date = {2020},
langid = {english},
note = {\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019JC016033},
keywords = {Gulf Stream, Lifespan of rings, Regime-Shift, Ring Census, size of rings, Warm Core Rings},
file = {Accepted Version:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\4GAVAJBF\\Gangopadhyay et al. - 2020 - A Census of the Warm-Core Rings of the Gulf Stream.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\8UCSFM2W\\2019JC016033.html:text/html},
}
@article{silver_forecasting_2021,
title = {Forecasting the Gulf Stream Path Using Buoyancy and Wind Forcing Over the North Atlantic},
volume = {126},
issn = {2169-9291},
url = {https://onlinelibrary.wiley.com/doi/abs/10.1029/2021JC017614},
doi = {10.1029/2021JC017614},
abstract = {Fluctuations in the path of the Gulf Stream ({GS}) have been previously studied by primarily connecting to either the wind-driven subtropical gyre circulation or buoyancy forcing via the subpolar gyre. Here we present a statistical model for 1 year predictions of the {GS} path (represented by the {GS} northern wall—{GSNW}) between W and W incorporating both mechanisms in a combined framework. An existing model with multiple parameters including the previous year's {GSNW} index, center location, and amplitude of the Icelandic Low and the Southern Oscillation Index was augmented with basin-wide Ekman drift over the Azores High. The addition of the wind is supported by a validation of the simpler two-layer Parsons-Veronis model of {GS} separation over the last 40 years. A multivariate analysis was carried out to compare 1-year-in-advance forecast correlations from four different models. The optimal predictors of the best performing model include: (a) the {GSNW} index from the previous year, (b) gyre-scale integrated Ekman Drift over the past 2 years, and (c) longitude of the Icelandic Low center lagged by 3 years. The forecast correlation over the 27 years (1994–2020) is 0.65, an improvement from the previous multi-parameter model's forecast correlation of 0.52. The improvement is attributed to the addition of the wind-drift component. The sensitivity of forecasting the {GS} path after extreme atmospheric years is quantified. Results indicate the possibility of better understanding and enhanced predictability of the dominant wind-driven variability of the Atlantic Meridional Overturning Circulation and of fisheries management models that use the {GS} path as a metric.},
pages = {e2021JC017614},
number = {8},
journaltitle = {Journal of Geophysical Research: Oceans},
author = {Silver, Adrienne and Gangopadhyay, Avijit and Gawarkiewicz, Glen and Taylor, Arnold and Sanchez-Franks, Alejandra},
urldate = {2022-02-10},
date = {2021},
langid = {english},
note = {\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JC017614},
keywords = {Gulf Stream, {AMOC}, Azores high, forecasting, Icelandic low, North Atlantic},
file = {Full Text:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\E6A2PALX\\Silver et al. - 2021 - Forecasting the Gulf Stream Path Using Buoyancy an.pdf:application/pdf;Snapshot:C\:\\Users\\joseph.caracappa\\Zotero\\storage\\RTB5CUQN\\2021JC017614.html:text/html},