Global synchrony of an accelerating rise in sea surface temperature
The oceans have shown a recent rapid and accelerating rise in temperature with, given the close link between temperature and marine organisms, pronounced effects on ecosystems. Here we describe for the first time a globally synchronous pattern of pulsed short period (~1 year long) emanations of warm...
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2012
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Online Access: | http://dx.doi.org/10.1017/s0025315412000549 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0025315412000549 |
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crcambridgeupr:10.1017/s0025315412000549 2024-10-06T13:52:43+00:00 Global synchrony of an accelerating rise in sea surface temperature Reid, Philip C. Beaugrand, Grégory 2012 http://dx.doi.org/10.1017/s0025315412000549 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0025315412000549 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of the Marine Biological Association of the United Kingdom volume 92, issue 7, page 1435-1450 ISSN 0025-3154 1469-7769 journal-article 2012 crcambridgeupr https://doi.org/10.1017/s0025315412000549 2024-09-11T04:04:34Z The oceans have shown a recent rapid and accelerating rise in temperature with, given the close link between temperature and marine organisms, pronounced effects on ecosystems. Here we describe for the first time a globally synchronous pattern of pulsed short period (~1 year long) emanations of warm sea surface temperature anomalies from tropical seas towards the poles on the shelf/slope with an intensification of the warming after the 1976/1977, 1986/1987 and 1997/1998 El Niños. On the eastern margins of continents the anomalies propagate towards the poles in part by largely baroclinic boundary currents, reinforced by regional atmospheric warming. The processes contributing to the less continuous warm anomalies on western margins are linked to the transfer of warmth from adjacent western boundary currents. These climate induced events show a close parallelism with the timing of ecosystem changes in shelf seas, important for fisheries and ecosystem services, and melting of sea-ice. Article in Journal/Newspaper Sea ice Cambridge University Press Journal of the Marine Biological Association of the United Kingdom 92 7 1435 1450 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
The oceans have shown a recent rapid and accelerating rise in temperature with, given the close link between temperature and marine organisms, pronounced effects on ecosystems. Here we describe for the first time a globally synchronous pattern of pulsed short period (~1 year long) emanations of warm sea surface temperature anomalies from tropical seas towards the poles on the shelf/slope with an intensification of the warming after the 1976/1977, 1986/1987 and 1997/1998 El Niños. On the eastern margins of continents the anomalies propagate towards the poles in part by largely baroclinic boundary currents, reinforced by regional atmospheric warming. The processes contributing to the less continuous warm anomalies on western margins are linked to the transfer of warmth from adjacent western boundary currents. These climate induced events show a close parallelism with the timing of ecosystem changes in shelf seas, important for fisheries and ecosystem services, and melting of sea-ice. |
format |
Article in Journal/Newspaper |
author |
Reid, Philip C. Beaugrand, Grégory |
spellingShingle |
Reid, Philip C. Beaugrand, Grégory Global synchrony of an accelerating rise in sea surface temperature |
author_facet |
Reid, Philip C. Beaugrand, Grégory |
author_sort |
Reid, Philip C. |
title |
Global synchrony of an accelerating rise in sea surface temperature |
title_short |
Global synchrony of an accelerating rise in sea surface temperature |
title_full |
Global synchrony of an accelerating rise in sea surface temperature |
title_fullStr |
Global synchrony of an accelerating rise in sea surface temperature |
title_full_unstemmed |
Global synchrony of an accelerating rise in sea surface temperature |
title_sort |
global synchrony of an accelerating rise in sea surface temperature |
publisher |
Cambridge University Press (CUP) |
publishDate |
2012 |
url |
http://dx.doi.org/10.1017/s0025315412000549 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0025315412000549 |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
Journal of the Marine Biological Association of the United Kingdom volume 92, issue 7, page 1435-1450 ISSN 0025-3154 1469-7769 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0025315412000549 |
container_title |
Journal of the Marine Biological Association of the United Kingdom |
container_volume |
92 |
container_issue |
7 |
container_start_page |
1435 |
op_container_end_page |
1450 |
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1812181181439934464 |