Compound high-temperature and low-chlorophyll extremes in the ocean over the satellite period
Extreme events in the ocean severely impact marine organisms and ecosystems. Of particular concern are compound events, i.e., when conditions are extreme for multiple potential ocean ecosystem stressors such as temperature and chlorophyll. Yet, little is known about the occurrence, intensity, and du...
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ftdoajarticles:oai:doaj.org/article:4fba592ebcb141938a05ab7176cbe7c2 2023-05-15T13:38:51+02:00 Compound high-temperature and low-chlorophyll extremes in the ocean over the satellite period N. Le Grix J. Zscheischler C. Laufkötter C. S. Rousseaux T. L. Frölicher 2021-03-01T00:00:00Z https://doi.org/10.5194/bg-18-2119-2021 https://doaj.org/article/4fba592ebcb141938a05ab7176cbe7c2 EN eng Copernicus Publications https://bg.copernicus.org/articles/18/2119/2021/bg-18-2119-2021.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-18-2119-2021 1726-4170 1726-4189 https://doaj.org/article/4fba592ebcb141938a05ab7176cbe7c2 Biogeosciences, Vol 18, Pp 2119-2137 (2021) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.5194/bg-18-2119-2021 2022-12-31T09:41:12Z Extreme events in the ocean severely impact marine organisms and ecosystems. Of particular concern are compound events, i.e., when conditions are extreme for multiple potential ocean ecosystem stressors such as temperature and chlorophyll. Yet, little is known about the occurrence, intensity, and duration of such compound high-temperature (a.k.a. marine heatwaves – MHWs) and low-chlorophyll (LChl) extreme events, whether their distributions have changed in the past decades, and what the potential drivers are. Here we use satellite-based sea surface temperature and chlorophyll concentration estimates to provide a first assessment of such compound extreme events. We reveal hotspots of compound MHW and LChl events in the equatorial Pacific, along the boundaries of the subtropical gyres, in the northern Indian Ocean, and around Antarctica. In these regions, compound events that typically last 1 week occur 3 to 7 times more often than expected under the assumption of independence between MHWs and LChl events. The occurrence of compound MHW and LChl events varies on seasonal to interannual timescales. At the seasonal timescale, most compound events occur in summer in both hemispheres. At the interannual timescale, the frequency of compound MHW and LChl events is strongly modulated by large-scale modes of natural climate variability such as the El Niño–Southern Oscillation, whose positive phase is associated with increased compound event occurrence in the eastern equatorial Pacific and in the Indian Ocean by a factor of up to 4. Our results provide a first understanding of where, when, and why compound MHW and LChl events occur. Further studies are needed to identify the exact physical and biological drivers of these potentially harmful events in the ocean and their evolution under global warming. Article in Journal/Newspaper Antarc* Antarctica Directory of Open Access Journals: DOAJ Articles Pacific Indian Biogeosciences 18 6 2119 2137 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
spellingShingle |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 N. Le Grix J. Zscheischler C. Laufkötter C. S. Rousseaux T. L. Frölicher Compound high-temperature and low-chlorophyll extremes in the ocean over the satellite period |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
Extreme events in the ocean severely impact marine organisms and ecosystems. Of particular concern are compound events, i.e., when conditions are extreme for multiple potential ocean ecosystem stressors such as temperature and chlorophyll. Yet, little is known about the occurrence, intensity, and duration of such compound high-temperature (a.k.a. marine heatwaves – MHWs) and low-chlorophyll (LChl) extreme events, whether their distributions have changed in the past decades, and what the potential drivers are. Here we use satellite-based sea surface temperature and chlorophyll concentration estimates to provide a first assessment of such compound extreme events. We reveal hotspots of compound MHW and LChl events in the equatorial Pacific, along the boundaries of the subtropical gyres, in the northern Indian Ocean, and around Antarctica. In these regions, compound events that typically last 1 week occur 3 to 7 times more often than expected under the assumption of independence between MHWs and LChl events. The occurrence of compound MHW and LChl events varies on seasonal to interannual timescales. At the seasonal timescale, most compound events occur in summer in both hemispheres. At the interannual timescale, the frequency of compound MHW and LChl events is strongly modulated by large-scale modes of natural climate variability such as the El Niño–Southern Oscillation, whose positive phase is associated with increased compound event occurrence in the eastern equatorial Pacific and in the Indian Ocean by a factor of up to 4. Our results provide a first understanding of where, when, and why compound MHW and LChl events occur. Further studies are needed to identify the exact physical and biological drivers of these potentially harmful events in the ocean and their evolution under global warming. |
format |
Article in Journal/Newspaper |
author |
N. Le Grix J. Zscheischler C. Laufkötter C. S. Rousseaux T. L. Frölicher |
author_facet |
N. Le Grix J. Zscheischler C. Laufkötter C. S. Rousseaux T. L. Frölicher |
author_sort |
N. Le Grix |
title |
Compound high-temperature and low-chlorophyll extremes in the ocean over the satellite period |
title_short |
Compound high-temperature and low-chlorophyll extremes in the ocean over the satellite period |
title_full |
Compound high-temperature and low-chlorophyll extremes in the ocean over the satellite period |
title_fullStr |
Compound high-temperature and low-chlorophyll extremes in the ocean over the satellite period |
title_full_unstemmed |
Compound high-temperature and low-chlorophyll extremes in the ocean over the satellite period |
title_sort |
compound high-temperature and low-chlorophyll extremes in the ocean over the satellite period |
publisher |
Copernicus Publications |
publishDate |
2021 |
url |
https://doi.org/10.5194/bg-18-2119-2021 https://doaj.org/article/4fba592ebcb141938a05ab7176cbe7c2 |
geographic |
Pacific Indian |
geographic_facet |
Pacific Indian |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Biogeosciences, Vol 18, Pp 2119-2137 (2021) |
op_relation |
https://bg.copernicus.org/articles/18/2119/2021/bg-18-2119-2021.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-18-2119-2021 1726-4170 1726-4189 https://doaj.org/article/4fba592ebcb141938a05ab7176cbe7c2 |
op_doi |
https://doi.org/10.5194/bg-18-2119-2021 |
container_title |
Biogeosciences |
container_volume |
18 |
container_issue |
6 |
container_start_page |
2119 |
op_container_end_page |
2137 |
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1766111605012037632 |