4.7 Article

Understanding the compound marine heatwave and low-chlorophyll extremes in the western Pacific Ocean

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FRONTIERS IN MARINE SCIENCE
卷 10, 期 -, 页码 -

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FRONTIERS MEDIA SA
DOI: 10.3389/fmars.2023.1303663

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western Pacific Ocean; marine heatwaves; low-chlorophyll; compound extreme events; multi-scale variability; climate change

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The western Pacific Ocean is highly vulnerable to climate change and serves as a global center for marine biodiversity. Understanding the spatial and temporal characteristics of compound marine heatwaves and low-chlorophyll extreme events is crucial for the conservation and management of marine organisms and ecosystems. The study finds that the South China Sea and Indonesian Seas are hotspots for compound events, with increasing frequency, intensity, and duration. Additionally, large-scale climate modes significantly influence the occurrence of these extreme events.
The western Pacific Ocean is the global center for marine biodiversity, with high vulnerability to climate change. A better understanding of the spatiotemporal characteristics and potential drivers of compound marine heatwaves (MHWs) and low-chlorophyll (LChl) extreme events is essential for the conservation and management of local marine organisms and ecosystems. Here, using daily satellite sea surface temperature and model-based chlorophyll concentration, we find that the climatological spatial distribution of MHW-LChl events in total days, duration, and intensity exhibits heterogeneous distributions. The southwest sections of the South China Sea (WSCS) and Indonesian Seas are the hotspots for compound events, with total MHW-LChl days that are more than 2.5 times higher than in the other sub-regions. Notably, there is a trend toward more frequent (> 4.2 d/decade), stronger (> 0.5), and longer-lasting (> 1.4 d/decade) MHW-LChl occurrences in the WSCS. The occurrence of compound MHW-LChl extremes exhibits remarkable seasonal differences, with the majority of these events transpiring during winter. Moreover, there are generally statistically significant increasing trends in MHW-LChl events for all properties on both seasonal and inter-annual timescales. Furthermore, we reveal that the total days of compound MHW-LChl extremes are strongly modulated by large-scale climate modes such as the El Nino-Southern Oscillation and Dipole Mode Index. Overall, pinpointing MHW-LChl hotspots and understanding their changes and drivers help vulnerable communities in better preparing for heightened and compounded risks to marine organism and ecosystems under climate change.

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