4.8 Article

Compound marine heatwaves and ocean acidity extremes

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NATURE COMMUNICATIONS
卷 13, 期 1, 页码 -

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NATURE PORTFOLIO
DOI: 10.1038/s41467-022-32120-7

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  1. Swiss National Science Foundation [PP00P2_198897]
  2. European Union [820989, 862923]
  3. Swiss National Science Foundation (SNF) [PP00P2_198897] Funding Source: Swiss National Science Foundation (SNF)

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This study shows that compound marine heatwave and ocean acidity extreme events have larger impacts on marine ecosystems than individual extremes. The likelihood of these compound events is higher in the subtropics and lower in the equatorial Pacific and mid-to-high latitudes. Climate change will increase the occurrence of compound events, leading to potentially severe impacts on marine ecosystems.
Compound MHW-OAX events, during which marine heatwaves (MHWs) co-occur with ocean acidity extreme (OAX) events, can have larger impacts on marine ecosystems than the individual extremes. Using monthly open-ocean observations over the period 1982-2019, we show that globally 1.8 in 100 months (or about one out of five present-day MHW months) are compound MHW-OAX event months under a present-day baseline, almost twice as many as expected for 90th percentile extreme event exceedances if MHWs and OAX events were statistically independent. Compound MHW-OAX events are most likely in the subtropics (2.7 in 100 months; 10 degrees-40 degrees latitude) and less likely in the equatorial Pacific and the mid-to-high latitudes (0.7 in 100 months; >40 degrees latitude). The likelihood pattern results from opposing effects of temperature and dissolved inorganic carbon on [H+]. The likelihood is higher where the positive effect on [H+] from increased temperatures during MHWs outweighs the negative effect on [H+] from co-occurring decreases in dissolved inorganic carbon. Daily model output from a large-ensemble simulation of an Earth system model is analyzed to assess changes in the MHW-OAX likelihood under climate change. The projected long-term mean warming and acidification trends have the largest effect on the number of MHW-OAX days per year, increasing it from 12 to 265 days per year at 2 degrees C global warming relative to a fixed pre-industrial baseline. Even when long-term trends are removed, an increase in [H+] variability leads to a 60% increase in the number of MHW-OAX days under 2 degrees C global warming. These projected increases may cause severe impacts on marine ecosystems. Compound extreme events in two or more oceanic ecosystem stressors are increasingly considered as a major concern for marine life. Here the authors present a first global analysis on compound marine heatwave and ocean acidity extreme events, identifying hotspots, drivers, and projecting future changes.

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