Climate change and dead zones

Estuaries and coastal seas provide valuable ecosystem services but are particularly vulnerable to the co-occurring threats of climate change and oxygen-depleted dead zones. We analyzed the severity of climate change predicted for existing dead zones, and found that 94% of dead zones are in regions t...

Full description

Bibliographic Details
Published in:Global Change Biology
Main Authors: Altieri, Andrew H., Gedan, Keryn B.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2015
Subjects:
Online Access:http://hdl.handle.net/10088/24372
https://doi.org/10.1111/gcb.12754
id ftsmithonian:oai:repository.si.edu:10088/24372
record_format openpolar
spelling ftsmithonian:oai:repository.si.edu:10088/24372 2023-05-15T17:51:19+02:00 Climate change and dead zones Altieri, Andrew H. Gedan, Keryn B. 2015 http://hdl.handle.net/10088/24372 https://doi.org/10.1111/gcb.12754 unknown Global Change Biology Altieri, Andrew H. and Gedan, Keryn B. 2015. "Climate change and dead zones." Global Change Biology . 21 (4):1395–1406. https://doi.org/10.1111/gcb.12754 1354-1013 http://hdl.handle.net/10088/24372 131065 doi:10.1111/gcb.12754 Journal Article 2015 ftsmithonian https://doi.org/10.1111/gcb.12754 2020-09-09T18:34:18Z Estuaries and coastal seas provide valuable ecosystem services but are particularly vulnerable to the co-occurring threats of climate change and oxygen-depleted dead zones. We analyzed the severity of climate change predicted for existing dead zones, and found that 94% of dead zones are in regions that will experience at least a 2 °C temperature increase by the end of the century. We then reviewed how climate change will exacerbate hypoxic conditions through oceanographic, ecological, and physiological processes. We found evidence that suggests numerous climate variables including temperature, ocean acidification, sea-level rise, precipitation, wind, and storm patterns will affect dead zones, and that each of those factors has the potential to act through multiple pathways on both oxygen availability and ecological responses to hypoxia. Given the variety and strength of the mechanisms by which climate change exacerbates hypoxia, and the rates at which climate is changing, we posit that climate change variables are contributing to the dead zone epidemic by acting synergistically with one another and with recognized anthropogenic triggers of hypoxia including eutrophication. This suggests that a multidisciplinary, integrated approach that considers the full range of climate variables is needed to track and potentially reverse the spread of dead zones. STRI Peer-reviewed Article in Journal/Newspaper Ocean acidification Unknown Global Change Biology 21 4 1395 1406
institution Open Polar
collection Unknown
op_collection_id ftsmithonian
language unknown
description Estuaries and coastal seas provide valuable ecosystem services but are particularly vulnerable to the co-occurring threats of climate change and oxygen-depleted dead zones. We analyzed the severity of climate change predicted for existing dead zones, and found that 94% of dead zones are in regions that will experience at least a 2 °C temperature increase by the end of the century. We then reviewed how climate change will exacerbate hypoxic conditions through oceanographic, ecological, and physiological processes. We found evidence that suggests numerous climate variables including temperature, ocean acidification, sea-level rise, precipitation, wind, and storm patterns will affect dead zones, and that each of those factors has the potential to act through multiple pathways on both oxygen availability and ecological responses to hypoxia. Given the variety and strength of the mechanisms by which climate change exacerbates hypoxia, and the rates at which climate is changing, we posit that climate change variables are contributing to the dead zone epidemic by acting synergistically with one another and with recognized anthropogenic triggers of hypoxia including eutrophication. This suggests that a multidisciplinary, integrated approach that considers the full range of climate variables is needed to track and potentially reverse the spread of dead zones. STRI Peer-reviewed
format Article in Journal/Newspaper
author Altieri, Andrew H.
Gedan, Keryn B.
spellingShingle Altieri, Andrew H.
Gedan, Keryn B.
Climate change and dead zones
author_facet Altieri, Andrew H.
Gedan, Keryn B.
author_sort Altieri, Andrew H.
title Climate change and dead zones
title_short Climate change and dead zones
title_full Climate change and dead zones
title_fullStr Climate change and dead zones
title_full_unstemmed Climate change and dead zones
title_sort climate change and dead zones
publishDate 2015
url http://hdl.handle.net/10088/24372
https://doi.org/10.1111/gcb.12754
genre Ocean acidification
genre_facet Ocean acidification
op_relation Global Change Biology
Altieri, Andrew H. and Gedan, Keryn B. 2015. "Climate change and dead zones." Global Change Biology . 21 (4):1395–1406. https://doi.org/10.1111/gcb.12754
1354-1013
http://hdl.handle.net/10088/24372
131065
doi:10.1111/gcb.12754
op_doi https://doi.org/10.1111/gcb.12754
container_title Global Change Biology
container_volume 21
container_issue 4
container_start_page 1395
op_container_end_page 1406
_version_ 1766158419699433472