Doubling of surface oceanic meridional heat transport by non-symmetry of mesoscale eddies

Abstract Oceanic transport of heat by ubiquitous mesoscale eddies plays a critical role in regulating climate variability and redistributing excess heat absorbed by ocean under global warming. Eddies have long been simplified as axisymmetric vortices and their influence on heat transport remains unc...

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Main Authors: Hailin Wang, Bo Qiu, Hanrui Liu, Zhengguang Zhang
Format: Article
Language:English
Published: Nature Portfolio 2023-09-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-023-41294-7
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author Hailin Wang
Bo Qiu
Hanrui Liu
Zhengguang Zhang
author_facet Hailin Wang
Bo Qiu
Hanrui Liu
Zhengguang Zhang
author_sort Hailin Wang
collection DOAJ
description Abstract Oceanic transport of heat by ubiquitous mesoscale eddies plays a critical role in regulating climate variability and redistributing excess heat absorbed by ocean under global warming. Eddies have long been simplified as axisymmetric vortices and their influence on heat transport remains unclear. Here, we combine satellite and drifter data and show that oceanic mesoscale eddies are asymmetric and directionally-dependent, and are controlled by their self-sustaining nature and their dynamical environment. Both the direction and amplitude of eddy-induced heat fluxes are significantly influenced by eddy’s asymmetry and directional dependence. When the eddy velocity field is decomposed into asymmetric and symmetric components, the eddy kinetic energy exhibits a nearly equal partition between these two components. The total eddy-induced meridional heat flux similarly doubles the heat flux induced by the symmetric components, highlighting the crucial contribution of eddy asymmetry on the magnitude of eddy-induced oceanic heat transport.
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spelling doaj.art-442117e2dbff4289847a2e1f17f72c2c2024-04-14T11:20:16ZengNature PortfolioNature Communications2041-17232023-09-0114111010.1038/s41467-023-41294-7Doubling of surface oceanic meridional heat transport by non-symmetry of mesoscale eddiesHailin Wang0Bo Qiu1Hanrui Liu2Zhengguang Zhang3Frontiers Science Center for Deep Ocean Multispheres and Earth System (FDOMES) and Key Laboratory of Physical Oceanography, Academy of the Future Ocean, Chongben Honors College, Ocean University of ChinaDepartment of Oceanography, University of Hawaii at ManoaFrontiers Science Center for Deep Ocean Multispheres and Earth System (FDOMES) and Key Laboratory of Physical Oceanography, Academy of the Future Ocean, Chongben Honors College, Ocean University of ChinaFrontiers Science Center for Deep Ocean Multispheres and Earth System (FDOMES) and Key Laboratory of Physical Oceanography, Academy of the Future Ocean, Chongben Honors College, Ocean University of ChinaAbstract Oceanic transport of heat by ubiquitous mesoscale eddies plays a critical role in regulating climate variability and redistributing excess heat absorbed by ocean under global warming. Eddies have long been simplified as axisymmetric vortices and their influence on heat transport remains unclear. Here, we combine satellite and drifter data and show that oceanic mesoscale eddies are asymmetric and directionally-dependent, and are controlled by their self-sustaining nature and their dynamical environment. Both the direction and amplitude of eddy-induced heat fluxes are significantly influenced by eddy’s asymmetry and directional dependence. When the eddy velocity field is decomposed into asymmetric and symmetric components, the eddy kinetic energy exhibits a nearly equal partition between these two components. The total eddy-induced meridional heat flux similarly doubles the heat flux induced by the symmetric components, highlighting the crucial contribution of eddy asymmetry on the magnitude of eddy-induced oceanic heat transport.https://doi.org/10.1038/s41467-023-41294-7
spellingShingle Hailin Wang
Bo Qiu
Hanrui Liu
Zhengguang Zhang
Doubling of surface oceanic meridional heat transport by non-symmetry of mesoscale eddies
Nature Communications
title Doubling of surface oceanic meridional heat transport by non-symmetry of mesoscale eddies
title_full Doubling of surface oceanic meridional heat transport by non-symmetry of mesoscale eddies
title_fullStr Doubling of surface oceanic meridional heat transport by non-symmetry of mesoscale eddies
title_full_unstemmed Doubling of surface oceanic meridional heat transport by non-symmetry of mesoscale eddies
title_short Doubling of surface oceanic meridional heat transport by non-symmetry of mesoscale eddies
title_sort doubling of surface oceanic meridional heat transport by non symmetry of mesoscale eddies
url https://doi.org/10.1038/s41467-023-41294-7
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AT zhengguangzhang doublingofsurfaceoceanicmeridionalheattransportbynonsymmetryofmesoscaleeddies