Future change in ocean productivity: Is the Arctic the new Atlantic?

One of the most characteristic features in ocean productivity is the North Atlantic spring bloom. Responding to seasonal increases in irradiance and stratification, surface phytopopulations rise significantly, a pattern that visibly tracks poleward into summer. While blooms also occur in the Arctic...

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Main Authors: Yool, A., Popova, E.E., Coward, A.C.
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Online Access:https://eprints.soton.ac.uk/385047/
https://eprints.soton.ac.uk/385047/1/Yool_et_al-Journal_of_Geophysical_Research__Oceans.pdf
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spelling ftsouthampton:oai:eprints.soton.ac.uk:385047 2023-07-30T03:59:46+02:00 Future change in ocean productivity: Is the Arctic the new Atlantic? Yool, A. Popova, E.E. Coward, A.C. 2015-12 text https://eprints.soton.ac.uk/385047/ https://eprints.soton.ac.uk/385047/1/Yool_et_al-Journal_of_Geophysical_Research__Oceans.pdf en English eng https://eprints.soton.ac.uk/385047/1/Yool_et_al-Journal_of_Geophysical_Research__Oceans.pdf Yool, A., Popova, E.E. and Coward, A.C. (2015) Future change in ocean productivity: Is the Arctic the new Atlantic? Journal of Geophysical Research: Oceans, 120 (12), 7771-7790. (doi:10.1002/2015JC011167 <http://dx.doi.org/10.1002/2015JC011167>). cc_by_4 Article PeerReviewed 2015 ftsouthampton 2023-07-09T22:03:24Z One of the most characteristic features in ocean productivity is the North Atlantic spring bloom. Responding to seasonal increases in irradiance and stratification, surface phytopopulations rise significantly, a pattern that visibly tracks poleward into summer. While blooms also occur in the Arctic Ocean, they are constrained by the sea-ice and strong vertical stratification that characterize this region. However, Arctic sea-ice is currently declining, and forecasts suggest this may lead to completely ice-free summers by the mid-21st century. Such change may open the Arctic up to Atlantic-style spring blooms, and do so at the same time as Atlantic productivity is threatened by climate change-driven ocean stratification. Here we use low and high-resolution instances of a coupled ocean-biogeochemistry model, NEMO-MEDUSA, to investigate productivity. Drivers of present-day patterns are identified, and changes in these across a climate change scenario (IPCC RCP 8.5) are analyzed. We find a globally significant decline in North Atlantic productivity (> ?20%) by 2100, and a correspondingly significant rise in the Arctic (> +50%). However, rather than the future Arctic coming to resemble the current Atlantic, both regions are instead transitioning to a common, low nutrient regime. The North Pacific provides a counterexample where nutrients remain high and productivity increases with elevated temperature. These responses to climate change in the Atlantic and Arctic are common between model resolutions, suggesting an independence from resolution for key impacts. However, some responses, such as those in the North Pacific, differ between the simulations, suggesting the reverse and supporting the drive to more fine-scale resolutions. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Climate change North Atlantic Sea ice University of Southampton: e-Prints Soton Arctic Arctic Ocean Pacific Medusa ENVELOPE(157.417,157.417,-79.633,-79.633)
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description One of the most characteristic features in ocean productivity is the North Atlantic spring bloom. Responding to seasonal increases in irradiance and stratification, surface phytopopulations rise significantly, a pattern that visibly tracks poleward into summer. While blooms also occur in the Arctic Ocean, they are constrained by the sea-ice and strong vertical stratification that characterize this region. However, Arctic sea-ice is currently declining, and forecasts suggest this may lead to completely ice-free summers by the mid-21st century. Such change may open the Arctic up to Atlantic-style spring blooms, and do so at the same time as Atlantic productivity is threatened by climate change-driven ocean stratification. Here we use low and high-resolution instances of a coupled ocean-biogeochemistry model, NEMO-MEDUSA, to investigate productivity. Drivers of present-day patterns are identified, and changes in these across a climate change scenario (IPCC RCP 8.5) are analyzed. We find a globally significant decline in North Atlantic productivity (> ?20%) by 2100, and a correspondingly significant rise in the Arctic (> +50%). However, rather than the future Arctic coming to resemble the current Atlantic, both regions are instead transitioning to a common, low nutrient regime. The North Pacific provides a counterexample where nutrients remain high and productivity increases with elevated temperature. These responses to climate change in the Atlantic and Arctic are common between model resolutions, suggesting an independence from resolution for key impacts. However, some responses, such as those in the North Pacific, differ between the simulations, suggesting the reverse and supporting the drive to more fine-scale resolutions.
format Article in Journal/Newspaper
author Yool, A.
Popova, E.E.
Coward, A.C.
spellingShingle Yool, A.
Popova, E.E.
Coward, A.C.
Future change in ocean productivity: Is the Arctic the new Atlantic?
author_facet Yool, A.
Popova, E.E.
Coward, A.C.
author_sort Yool, A.
title Future change in ocean productivity: Is the Arctic the new Atlantic?
title_short Future change in ocean productivity: Is the Arctic the new Atlantic?
title_full Future change in ocean productivity: Is the Arctic the new Atlantic?
title_fullStr Future change in ocean productivity: Is the Arctic the new Atlantic?
title_full_unstemmed Future change in ocean productivity: Is the Arctic the new Atlantic?
title_sort future change in ocean productivity: is the arctic the new atlantic?
publishDate 2015
url https://eprints.soton.ac.uk/385047/
https://eprints.soton.ac.uk/385047/1/Yool_et_al-Journal_of_Geophysical_Research__Oceans.pdf
long_lat ENVELOPE(157.417,157.417,-79.633,-79.633)
geographic Arctic
Arctic Ocean
Pacific
Medusa
geographic_facet Arctic
Arctic Ocean
Pacific
Medusa
genre Arctic
Arctic
Arctic Ocean
Climate change
North Atlantic
Sea ice
genre_facet Arctic
Arctic
Arctic Ocean
Climate change
North Atlantic
Sea ice
op_relation https://eprints.soton.ac.uk/385047/1/Yool_et_al-Journal_of_Geophysical_Research__Oceans.pdf
Yool, A., Popova, E.E. and Coward, A.C. (2015) Future change in ocean productivity: Is the Arctic the new Atlantic? Journal of Geophysical Research: Oceans, 120 (12), 7771-7790. (doi:10.1002/2015JC011167 <http://dx.doi.org/10.1002/2015JC011167>).
op_rights cc_by_4
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