Article (Scientific journals)
Arctic and Subarctic marine heatwaves and their ecological impacts
Pecuchet, Laurene; Mohamed, Bayoumy Abdelaziz; Hayward, Alexander et al.
2025In Frontiers in Environmental Science, 13
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Abstract :
[en] The Arctic and Subarctic seas are predicted to become hotspots for marine heatwaves (MHWs). High-latitude marine ecosystems face unique consequences from accelerated warming and sea ice loss, challenging species adapted to cold conditions. We review the literature on MHW characteristics and ecological impacts in the Arctic and Subarctic seas, and contrast MHW characteristics between the Bering Sea and Barents Sea. We uncover the pervasive impacts of MHWs across widely different organism groups, including benthic foundation species, phytoplankton, zooplankton, fish, seabirds, and marine mammals. MHWs in the Arctic marginal seas are especially prevalent in areas experiencing sea ice retreat, such as seasonal sea ice zones, highlighting the complex interplay between MHWs and sea ice dynamics. Overall, few studies have documented the ecological impacts of MHWs on high-latitude ecosystems, with the notable exception of the impacts from the Bering Sea and Chukchi Sea MHWs in 2017–2019. Many Arctic species, with their cold and narrow thermal preferences, appear vulnerable to MHWs, as they might not have access to cold climate refugia, while boreal species appear to benefit from Arctic and Subarctic MHWs. Sessile foundation species, such as kelp and seagrasses, are especially at risk during MHWs, although in the Arctic evidence of MHWs impacts remains limited. Reproductive failure and mass mortality events have been documented for several species in the Pacific Arctic (e.g., seabirds, fish, crabs). MHWs have been observed to have ecosystem-wide repercussions in the northern Bering Sea and Chukchi Sea with shifts in plankton communities affecting the entire food web. The ecological responses to MHWs in the Arctic and Subarctic ecosystems are still not fully understood, highlighting a need for further research to assess the direct and indirect impacts on various taxa and to improve predictive models for better management and conservation strategies. MHWs can also have large consequences for ecosystem services and socio-ecological systems, for example, closures of economically valuable and culturally important fisheries, as seen in Alaska, degradation of traditional ice-hunting practices, and compromised wellbeing of coastal communities. Large and abrupt ecosystem changes following MHWs underscore the urgent need for adaptive management strategies in the face of ongoing climate change.
Precision for document type :
Review article
Disciplines :
Earth sciences & physical geography
Author, co-author :
Pecuchet, Laurene
Mohamed, Bayoumy Abdelaziz  ;  Université de Liège - ULiège > Freshwater and OCeanic science Unit of reSearch (FOCUS)
Hayward, Alexander
Alvera Azcarate, Aida  ;  Université de Liège - ULiège > Département d'astrophysique, géophysique et océanographie (AGO) > GeoHydrodynamics and Environment Research (GHER)
Dörr, Jakob
Filbee-Dexter, Karen
Kuletz, Katherine J.
Luis, Kelly
Manizza, Manfredi
Miller, Charles E.
Staehr, Peter A. U.
Szymkowiak, Marysia
Wernberg, Thomas
More authors (3 more) Less
Language :
English
Title :
Arctic and Subarctic marine heatwaves and their ecological impacts
Publication date :
19 February 2025
Journal title :
Frontiers in Environmental Science
eISSN :
2296-665X
Publisher :
Frontiers
Volume :
13
Peer reviewed :
Peer Reviewed verified by ORBi
European Projects :
HE - 101059823 - B-USEFUL - User-oriented Solutions for Improved Monitoring and Management of Biodiversity and Ecosystem services in vulnerable European Seas
HE - 101060072 - ACTNOW - Advancing understanding of Cumulative Impacts on European marine biodiversity, ecosystem functions and services for human wellbeing
Funders :
ERC - European Research Council
Funding text :
The author(s) declare that financial support was received for the research, authorship, and/or publication of this article. LP acknowledges financial support from the European Union’s Horizon Europe research and innovation program project “BUSEFUL” (ID:101059823) and “ACTNOW” (ID:101060072). BM and AA-A (University of Liège) acknowledge financial support from the STEREO-IV (Support To Exploitation and Research in Earth Observation) program administered by BELSPO (Belgian Science Policy Office) through the North-Heat project (STEREO-IV BELSPO # project SR/00/404). MM acknowledges financial support from the National Science Foundation (OPP- 1922922) and from NASA (IDS19-0113).
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