Vertical structures of marine heatwaves

Abstract A marine heatwave (MHW) is typically defined as an anomalous warm event in the surface ocean, with wide-ranging impacts on marine and socio-economic systems. The surface warming associated with MHWs can penetrate into the deep ocean; however, the vertical structure of MHWs is poorly known i...

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Main Authors: Ying Zhang, Yan Du, Ming Feng, Alistair J. Hobday
Format: Article
Language:English
Published: Nature Portfolio 2023-10-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-023-42219-0
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author Ying Zhang
Yan Du
Ming Feng
Alistair J. Hobday
author_facet Ying Zhang
Yan Du
Ming Feng
Alistair J. Hobday
author_sort Ying Zhang
collection DOAJ
description Abstract A marine heatwave (MHW) is typically defined as an anomalous warm event in the surface ocean, with wide-ranging impacts on marine and socio-economic systems. The surface warming associated with MHWs can penetrate into the deep ocean; however, the vertical structure of MHWs is poorly known in the global ocean. Here, we identify four main types of MHWs with different vertical structures using Argo profiles: shallow, subsurface-reversed, subsurface-intensified, and deep MHWs. These MHW types are characterized by different spatial distributions with hotspots of subsurface-reversed and subsurface-intensified MHWs at low latitudes and shallow and deep MHWs at middle-high latitudes. These vertical structures are influenced by ocean dynamical processes, including oceanic planetary waves, boundary currents, eddies, and mixing. The area and depth of all types of MHWs exhibit significant increasing trends over the past two decades. These results contribute to a better understanding of the physical drivers and ecological impacts of MHWs in a warming climate.
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spelling doaj.art-158626ed057c4e0b974a29569b10a2ab2023-11-20T10:11:29ZengNature PortfolioNature Communications2041-17232023-10-0114111210.1038/s41467-023-42219-0Vertical structures of marine heatwavesYing Zhang0Yan Du1Ming Feng2Alistair J. Hobday3State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of SciencesState Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of SciencesCSIRO EnvironmentCSIRO EnvironmentAbstract A marine heatwave (MHW) is typically defined as an anomalous warm event in the surface ocean, with wide-ranging impacts on marine and socio-economic systems. The surface warming associated with MHWs can penetrate into the deep ocean; however, the vertical structure of MHWs is poorly known in the global ocean. Here, we identify four main types of MHWs with different vertical structures using Argo profiles: shallow, subsurface-reversed, subsurface-intensified, and deep MHWs. These MHW types are characterized by different spatial distributions with hotspots of subsurface-reversed and subsurface-intensified MHWs at low latitudes and shallow and deep MHWs at middle-high latitudes. These vertical structures are influenced by ocean dynamical processes, including oceanic planetary waves, boundary currents, eddies, and mixing. The area and depth of all types of MHWs exhibit significant increasing trends over the past two decades. These results contribute to a better understanding of the physical drivers and ecological impacts of MHWs in a warming climate.https://doi.org/10.1038/s41467-023-42219-0
spellingShingle Ying Zhang
Yan Du
Ming Feng
Alistair J. Hobday
Vertical structures of marine heatwaves
Nature Communications
title Vertical structures of marine heatwaves
title_full Vertical structures of marine heatwaves
title_fullStr Vertical structures of marine heatwaves
title_full_unstemmed Vertical structures of marine heatwaves
title_short Vertical structures of marine heatwaves
title_sort vertical structures of marine heatwaves
url https://doi.org/10.1038/s41467-023-42219-0
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