Global-scale random bottom pressure fluctuations from oceanic intrinsic variability

International audience Intrinsic processes such as mesoscale turbulence have recently been proved as important as atmospheric variability in causing variations in ocean bottom pressure (p b). Intrinsic processes are also known to generate random variability on scales larger than the mesoscale throug...

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Bibliographic Details
Main Authors: Zhao, Mengnan, Ponte, Rui, Penduff, Thierry
Other Authors: Atmospheric and Environmental Research, Inc. (AER), Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Observatoire des Sciences de l'Univers de Grenoble (Fédération OSUG)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP), Université Grenoble Alpes (UGA)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2023
Subjects:
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
Arctic
Drake Passage
Southern Ocean
Atlantic Arctic
Atlantic-Arctic
Online Access:https://hal.science/hal-04213103
https://hal.science/hal-04213103v1/document
https://hal.science/hal-04213103v1/file/Zhao2023.pdf
https://doi.org/10.1126/sciadv.adg02
Description
Summary:International audience Intrinsic processes such as mesoscale turbulence have recently been proved as important as atmospheric variability in causing variations in ocean bottom pressure (p b). Intrinsic processes are also known to generate random variability on scales larger than the mesoscale through inverse energy cascades or large-scale baroclinic instability. Here, model analyses reveal a truly global-scale, intrinsic p b mode of variability at monthly time scales that relies on a different mechanism. The intrinsic mode has largest amplitudes around Drake Passage and opposite polarity between the Southern Ocean and Atlantic/Arctic oceans. Its signature is consistent with localized eddy-driven p b anomalies of opposite sign near Drake Passage that then adjust freely in the rest of the ocean via barotropic wave processes. This intrinsic mode seems consistent with observed p b variability.

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