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Surface and Subsurface Compound MHW and Biogeochemical Extremes Under Climate Change

Natacha, Le Grix

Abstract

Overview Climate coffee with Natacha Legrix De La Salle (Univ. Liverpool) held on 27 November 2025 Abstract. Marine species are increasingly threatened by extreme and compound events, as warming, deoxygenation, and acidification unfold. Yet, the surface and especially the subsurface distribution and evolution of such compound events remain poorly understood. We present the current and projected distributions of compound marine heatwave (MHW), low oxygen (LOX), and high acidity (OAX) events throughout the water column, using observation‐based data from 2004 to 2019 and large ensemble Earth system model simulations from 1890 to 2100. Our findings reveal that compound MHW‐OAX and OAX‐LOX events are prevalent in the low to mid latitudes at the ocean surface. At 200 and 600 m, MHW‐OAX and MHW‐LOX events are frequent in the high latitudes and parts of the tropics, while OAX‐LOX events occur globally. Subsurface compound events are often associated with vertical displacements of water masses, with the climatological vertical gradients of ecosystem stressors typically explaining their occurrence patterns. Projections show a strong rise in compound event frequency over the historical period and under continued global warming, primarily driven by shifts in mean oceanic conditions. The portion of the top 2,000 m affected by extreme or compound events rises from 20% to 98% under 2°C of global warming in a high emissions scenario using a preindustrial baseline, and to 30% using a shifting‐mean baseline. However, physical and biogeochemical changes may lead to regional decreases in subsurface events, highlighting complexities in how warming, deoxygenation, and ocean acidification unfold in the ocean interior. Increasing compound event frequency poses a major threat to marine ecosystems, potentially disrupting food webs and biodiversity. Paper https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2025GB008514 Our speaker Natacha Legrix De La Salle (Univ. Bern) What is a Climate Coffee? #climatecoffees are short (circa 40 min: 20 min talk + 20 min Q&A), relaxed meetings for scientists to share ideas, discuss methods, and communicate new results. They are open to speakers of all seniority; we especially encourage early-career scientists to become speakers. The Coffees are an exciting opportunity for scientists to build a network and disseminate recent results peer-to-peer. We invite researchers from across the climate science community to join us for this series of regular online knowledge exchange events. Organisation The Climate Coffees are organized by the Horizon Europe projects TipESM, ObsSea4Clim, OCEAN ICE, the National Center for Climate Research - DMI of the Danish Meteorological Institute and the European Climate Research Alliance. Disclaimer Funded by the European Union. Views and opinions expressed are however those of the author(s) only and do not necessarily reflect those of the European Union or is agencies CINEA and REA. Neither the European Union nor the granting authority can be held responsible for them.

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27 November 2025 | 10:00 Climate Coffee Capotondi et al. (2024) Motivation Marine heatwaves can be biological game changers 1 Wernberg et al. (2016) Motivation Yet not all marine heatwaves are harmful 2 Fredston et al. (2023) Role of compound events? Le Grix et al. (2023) Motivation Compound events are often associated with severe impacts 3 Capotondi et al. (2024) Motivation Compound events are often associated with severe impacts 4 Gruber, Boyd, Frölicher, Vogt (2021) Years Heatwave Low oxygen High acidity Heatwave Low oxygen Heatwave Heatwave Low oxygen Heatwave Heatwave High acidity The ‘Blob’ Area affected (%) Research questions 1. Where do marine heatwaves, high acidity and low oxygen extreme events tend to co-occur? 2. How can we explain their compound event frequency patterns? 3. How will they evolve under climate change? 5 Methods •Model: GFDL-ESM2M-LE (15 ensemble members; 1891-2100 following RCP8.5; daily-mean output) •Observations: NOAA OISST, MOBO-DIC, GOBAI-O2 •Ecosystem stressors: high T (MHW), high H+ (OAX), low O2 (LOX) •Definition of extremes: seasonally varying 90th or 10th percentile threshold •Focus on multivariate compound events, i.e., extreme events on the same day and location. Top 2000 m 6 MHW-OAX-LOX Results more frequent than expectedless frequent than expected Present-day distribution of compound extreme events 7 MHW-OAX-LOX Results more frequent than expectedless frequent than expected MHW-OAX-LOX Present-day distribution of compound extreme events 8 MHW-OAX MHW-LOX OAX-LOX Mean + Variability + Dependence Under a fixed baseline: Strongest increase at the sea surface for all compound event types. In 2100 at surface (RCP8.5): Compound MHW-OAX, MHW-LOX and OAX-LOX events occur in more than 80% of days Results Historical and future changes in compound event frequency Fixed 13 Results 25 Mean + Variability + Dependence Variability + Dependence Dependence MHW-OAX MHW-LOX OAX-LOX Historical and future changes in compound event frequency Fixed Shifting-mean Fully-adapting 14 Results 25 Mean + Variability + Dependence Variability + Dependence Dependence MHW-OAX MHW-LOX OAX-LOX Historical and future changes in compound event frequency Most of the frequency increase is driven by long-term mean shifts in T, H+ and O2 Shifting-mean Fully-adapting Fixed 14 Results In some regions, subsurface MHW-OAX events do not increase or even decrease Complexities in how warming and acidification unfold in the ocean interior.  25 MHW-OAX MHW-LOX OAX-LOX Historical and future changes in compound event frequency Shifting-mean Fully-adapting Fixed * *617m 15 MHW-OAX-LOX 2°C warming 98% Under fixed preindustrial baseline Results 98% of top 2000m exposed to extreme/compound events under 2°C Under shifting baseline MHW-OAX-LOX Under a fixed preindustrial baseline 30% Historical and future changes in compound event frequency 16 MHW-OAX-LOX 2°C warming 98% Under fixed preindustrial baseline Results 98% of top 2000m exposed to extreme/compound events under 2°C Under shifting baseline MHW-OAX-LOX 98% Under a fixed preindustrial baseline 30% 98% of global ocean volume down to 2000m will be exposed to an extreme/compound event under 2°C warming. Historical and future changes in compound event frequency 16 MHW-OAX-LOX 2°C warming 98% Under fixed preindustrial baseline Results 98% of top 2000m exposed to extreme/compound events under 2°C Under shifting baseline MHW-OAX-LOX 98% Under a shifting baseline 30% Under a fixed preindustrial baseline Historical and future changes in compound event frequency 16 •Extreme conditions in T, H+ and O2 frequently coincide at the sea surface and in large parts of the subsurface ocean. •Subsurface compound events are often linked to vertical water mass shifts. •The projected rise in compound events under climate change occurs in most of the global ocean down to 2000 m. Take-home messages Density anomaly (kg/m3) 17