Arctic Amplification of marine heatwaves under global warming

Marine heatwaves (MHWs) and total heat exposures (THEs), extreme warming events occurring across the global oceans, seriously threaten marine ecosystems and coastal communities as the climate warms. However, future changes in MHWs and THEs in the Arctic Ocean, where unique marine ecosystems are present, are still unclear. Here, based on the latest CMIP6 climate simulations, we find that both MHWs and THEs in the Arctic Ocean are anticipated to intensify in a warming climate, mainly due to Arctic sea ice decline and long-term warming trend, respectively. Particularly striking is the projected rise in MHW mean intensity during the 21<sup>st</sup> century in the Arctic Ocean, surpassing the global average by more than sevenfold under the CMIP6 SSP585 scenario. This phenomenon, coined the 'Arctic MHW Amplification', underscores an impending and disproportionately elevated threat to the Arctic marine life, necessitating targeted conservation and adaptive strategies.

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Publication Details

Journal
Nature Communications
Published
2024-09-26
DOI
https://doi.org/10.1038/s41467-024-52760-1
Citations
20
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
7.53

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article

Arctic Amplification of marine heatwaves under global warming

Zhenya Song, Qi Shu, Qiang Wang, Yan He et al.
20 citations
Nature Communications
Arctic and Antarctic ice dynamics
7.53
article

Arctic Amplification of marine heatwaves under global warming

Zhenya Song, Qi Shu, Qiang Wang, Yan He, Fangli Qiao, Shizhu Wang, Min Zhang, Lujun Zhang, Haibo Bi, Rongrong Pan
article en
20 citations

Abstract

Marine heatwaves (MHWs) and total heat exposures (THEs), extreme warming events occurring across the global oceans, seriously threaten marine ecosystems and coastal communities as the climate warms. However, future changes in MHWs and THEs in the Arctic Ocean, where unique marine ecosystems are present, are still unclear. Here, based on the latest CMIP6 climate simulations, we find that both MHWs and THEs in the Arctic Ocean are anticipated to intensify in a warming climate, mainly due to Arctic sea ice decline and long-term warming trend, respectively. Particularly striking is the projected rise in MHW mean intensity during the 21<sup>st</sup> century in the Arctic Ocean, surpassing the global average by more than sevenfold under the CMIP6 SSP585 scenario. This phenomenon, coined the 'Arctic MHW Amplification', underscores an impending and disproportionately elevated threat to the Arctic marine life, necessitating targeted conservation and adaptive strategies.

Nature CommunicationsVol. 15(1)
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), Chinese Academy of Sciences (CN), Ministry of Natural Resources (CN), Institute of Oceanology (CN), Qingdao National Laboratory for Marine Science and Technology (CN), First Institute of Oceanography (CN), Numerical Method (China) (CN), Nanjing University (CN)
National Natural Science Foundation of China, Natural Science Foundation of Shandong Province, National Key Research and Development Program of China
Life below water
Openalex Percentile: Top 2%
Arctic and Antarctic ice dynamics
7.53
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