Author
Listed:
- Xiuwen Guo
(Ocean University of China)
- Yang Gao
(Ocean University of China
Qingdao National Laboratory for Marine Science and Technology
International Laboratory for High‐Resolution Earth System Prediction (iHESP))
- Shaoqing Zhang
(Qingdao National Laboratory for Marine Science and Technology
International Laboratory for High‐Resolution Earth System Prediction (iHESP)
Ocean University of China)
- Lixin Wu
(International Laboratory for High‐Resolution Earth System Prediction (iHESP)
Ocean University of China)
- Ping Chang
(International Laboratory for High‐Resolution Earth System Prediction (iHESP)
Texas A&M University)
- Wenju Cai
(CSIRO Oceans and Atmosphere
Ocean University of China and Pilot National Laboratory for Marine Science and Technology (Qingdao))
- Jakob Zscheischler
(Helmholtz Centre for Environmental Research – UFZ
University of Bern
University of Bern)
- L. Ruby Leung
(Pacific Northwest National Laboratory)
- Justin Small
(International Laboratory for High‐Resolution Earth System Prediction (iHESP)
National Center for Atmospheric Research)
- Gokhan Danabasoglu
(International Laboratory for High‐Resolution Earth System Prediction (iHESP)
National Center for Atmospheric Research)
- Luanne Thompson
(University of Washington)
- Huiwang Gao
(Ocean University of China)
Abstract
Marine heatwaves (MHWs), episodic periods of abnormally high sea surface temperature, severely affect marine ecosystems. Large marine ecosystems (LMEs) cover ~22% of the global ocean but account for 95% of global fisheries catches. Yet how climate change affects MHWs over LMEs remains unknown because such LMEs are confined to the coast where low-resolution climate models are known to have biases. Here, using a high-resolution Earth system model and applying a ‘future threshold’ that considers MHWs as anomalous warming above the long-term mean warming of sea surface temperatures, we find that future intensity and annual days of MHWs over the majority of the LMEs remain higher than in the present-day climate. Better resolution of ocean mesoscale eddies enables simulation of more realistic MHWs than low-resolution models. These increases in MHWs under global warming pose a serious threat to LMEs, even if resident organisms could adapt fully to the long-term mean warming.
Suggested Citation
Xiuwen Guo & Yang Gao & Shaoqing Zhang & Lixin Wu & Ping Chang & Wenju Cai & Jakob Zscheischler & L. Ruby Leung & Justin Small & Gokhan Danabasoglu & Luanne Thompson & Huiwang Gao, 2022.
"Threat by marine heatwaves to adaptive large marine ecosystems in an eddy-resolving model,"
Nature Climate Change, Nature, vol. 12(2), pages 179-186, February.
Handle:
RePEc:nat:natcli:v:12:y:2022:i:2:d:10.1038_s41558-021-01266-5
DOI: 10.1038/s41558-021-01266-5
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Cited by:
- Alex S. J. Wyatt & James J. Leichter & Libe Washburn & Li Kui & Peter J. Edmunds & Scott C. Burgess, 2023.
"Hidden heatwaves and severe coral bleaching linked to mesoscale eddies and thermocline dynamics,"
Nature Communications, Nature, vol. 14(1), pages 1-17, December.
- Changyu Li & Jianping Huang & Xiaoyue Liu & Lei Ding & Yongli He & Yongkun Xie, 2024.
"The ocean losing its breath under the heatwaves,"
Nature Communications, Nature, vol. 15(1), pages 1-11, December.
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