Under pressure: Climate change, upwelling and eastern boundary upwelling ecosystems

The IPCC AR5 provided an overview of the likely effects of climate change on Eastern Boundary Upwelling Systems (EBUS), stimulating increased interest in research examining the issue. We use these recent studies to develop a new synthesis describing climate change impacts on EBUS. We find that mod...

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Main Authors: Marisol eGarcía-Reyes, William J Sydeman, David S Schoeman, Ryan R Rykaczewski, Bryan A Black, Albertus J Smit, Steven J Bograd
Format: Article
Language:English
Published: Frontiers Media S.A. 2015-12-01
Series:Frontiers in Marine Science
Subjects:
Online Access:http://journal.frontiersin.org/Journal/10.3389/fmars.2015.00109/full
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author Marisol eGarcía-Reyes
William J Sydeman
David S Schoeman
Ryan R Rykaczewski
Bryan A Black
Albertus J Smit
Steven J Bograd
author_facet Marisol eGarcía-Reyes
William J Sydeman
David S Schoeman
Ryan R Rykaczewski
Bryan A Black
Albertus J Smit
Steven J Bograd
author_sort Marisol eGarcía-Reyes
collection DOAJ
description The IPCC AR5 provided an overview of the likely effects of climate change on Eastern Boundary Upwelling Systems (EBUS), stimulating increased interest in research examining the issue. We use these recent studies to develop a new synthesis describing climate change impacts on EBUS. We find that model and observational data suggest coastal upwelling-favorable winds in poleward portions of EBUS have intensified and will continue to do so in the future. Although evidence is weak in data that are presently available, future projections show that this pattern might be driven by changes in the positioning of the oceanic high-pressure systems rather than by deepening of the continental low-pressure systems, as previously proposed. There is low confidence regarding the future effects of climate change on coastal temperatures and biogeochemistry due to uncertainty in the countervailing responses to increasing upwelling and coastal warming, the latter of which could increase thermal stratification and render upwelling less effective in lifting nutrient-rich deep waters into the photic zone. Although predictions of ecosystem responses are uncertain, EBUS experience considerable natural variability and may be inherently resilient. However, multi-trophic level, end-to-end (i.e., winds to whales) studies are needed to resolve the resilience of EBUS to climate change, especially their response to long-term trends or extremes that exceed pre-industrial ranges.
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spelling doaj.art-519dacc1973141578c0796cc2e372e432022-12-22T00:53:08ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452015-12-01210.3389/fmars.2015.00109158974Under pressure: Climate change, upwelling and eastern boundary upwelling ecosystemsMarisol eGarcía-Reyes0William J Sydeman1David S Schoeman2Ryan R Rykaczewski3Bryan A Black4Albertus J Smit5Steven J Bograd6Farallon Institute for Advanced Ecosystem ResearchFarallon Institute for Advanced Ecosystem ResearchUniversity of the Sunshine CoastUniversity of South CarolinaUniversity of TexasUniversity of the Western CapeNOAA Southwest Fisheries Science CenterThe IPCC AR5 provided an overview of the likely effects of climate change on Eastern Boundary Upwelling Systems (EBUS), stimulating increased interest in research examining the issue. We use these recent studies to develop a new synthesis describing climate change impacts on EBUS. We find that model and observational data suggest coastal upwelling-favorable winds in poleward portions of EBUS have intensified and will continue to do so in the future. Although evidence is weak in data that are presently available, future projections show that this pattern might be driven by changes in the positioning of the oceanic high-pressure systems rather than by deepening of the continental low-pressure systems, as previously proposed. There is low confidence regarding the future effects of climate change on coastal temperatures and biogeochemistry due to uncertainty in the countervailing responses to increasing upwelling and coastal warming, the latter of which could increase thermal stratification and render upwelling less effective in lifting nutrient-rich deep waters into the photic zone. Although predictions of ecosystem responses are uncertain, EBUS experience considerable natural variability and may be inherently resilient. However, multi-trophic level, end-to-end (i.e., winds to whales) studies are needed to resolve the resilience of EBUS to climate change, especially their response to long-term trends or extremes that exceed pre-industrial ranges.http://journal.frontiersin.org/Journal/10.3389/fmars.2015.00109/fullstratificationClimate change impactsUpwelling intensificationupwelling driversgeneral circulation model projections
spellingShingle Marisol eGarcía-Reyes
William J Sydeman
David S Schoeman
Ryan R Rykaczewski
Bryan A Black
Albertus J Smit
Steven J Bograd
Under pressure: Climate change, upwelling and eastern boundary upwelling ecosystems
Frontiers in Marine Science
stratification
Climate change impacts
Upwelling intensification
upwelling drivers
general circulation model projections
title Under pressure: Climate change, upwelling and eastern boundary upwelling ecosystems
title_full Under pressure: Climate change, upwelling and eastern boundary upwelling ecosystems
title_fullStr Under pressure: Climate change, upwelling and eastern boundary upwelling ecosystems
title_full_unstemmed Under pressure: Climate change, upwelling and eastern boundary upwelling ecosystems
title_short Under pressure: Climate change, upwelling and eastern boundary upwelling ecosystems
title_sort under pressure climate change upwelling and eastern boundary upwelling ecosystems
topic stratification
Climate change impacts
Upwelling intensification
upwelling drivers
general circulation model projections
url http://journal.frontiersin.org/Journal/10.3389/fmars.2015.00109/full
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