Preprints
https://doi.org/10.5194/egusphere-2025-5296
https://doi.org/10.5194/egusphere-2025-5296
21 Dec 2025
 | 21 Dec 2025
Status: this preprint is open for discussion and under review for Earth System Dynamics (ESD).

Underestimated Future Arctic Ocean Warming due to Unresolved Marine Heatwaves at Low Resolution

Ruijian Gou, Yaocheng Deng, Yingzhe Cui, Qi Shu, Hong Wang, Shengpeng Wang, Lixin Wu, and Gerrit Lohmann

Abstract. The Arctic Ocean is projected to warm twice more than the global mean in a warming 21st century, following increased solar heat input due to sea ice decrease. Here we find that this increase in solar heat input is larger in a higher-resolution climate model compared to a low-resolution one. This is due to the impacts of Arctic marine heatwaves (MHWs), known as episodes of extreme ocean warming. The explicit consideration of MHWs, which are stronger and more realistic in higher-resolution models, increases melting of sea ice and thus solar heat input, thereby reinforcing the long-term Arctic Ocean warming. A positive feedback is identified between stronger MHWs and larger Arctic Ocean warming. We emphasize that Arctic Ocean warming is underestimated by the current generation of climate models, which generally have a too low spatial resolution to resolve Arctic MHWs. We conclude that future eddy- and storm-resolving models will provide a new perspective on the Earth system's response to past and future climate and environmental extremes.

Competing interests: Gerrit Lohmann is a member of the editorial board of ESD.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Ruijian Gou, Yaocheng Deng, Yingzhe Cui, Qi Shu, Hong Wang, Shengpeng Wang, Lixin Wu, and Gerrit Lohmann

Status: open (until 01 Feb 2026)

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Ruijian Gou, Yaocheng Deng, Yingzhe Cui, Qi Shu, Hong Wang, Shengpeng Wang, Lixin Wu, and Gerrit Lohmann
Ruijian Gou, Yaocheng Deng, Yingzhe Cui, Qi Shu, Hong Wang, Shengpeng Wang, Lixin Wu, and Gerrit Lohmann

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Short summary
Under anthropogenic warming, Arctic warming is nearly four times faster than global average. One key reason is the ice-albedo feedback – sea ice melting reveals the darker ocean water, which absorbs more solar radiation. Using a climate model of more refined grids, we find that the ocean absorbs more solar radiation. We attribute it to the better represented short-term extreme ocean warming events. They cause more short-term sea ice melting, allowing the ocean to absorb more solar radiation.
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