Upstream and Downstream Wind‐Stress Forcing of Seasonal Variability of Luzon Strait Deep Overflow Transport

Abstract The Luzon Strait Deep Overflow (LZDO) transports deep‐water masses from the Pacific Ocean (upstream) to the South China Sea (SCS, downstream), playing a vital role in shaping the hydrographic and biogeochemical structure and regulating abyssal circulation within the SCS. Recent studies sugg...

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Main Authors: Lei Chen, Jiayan Yang, Lixin Wu
Format: Article
Language:English
Published: Wiley 2025-01-01
Series:Geophysical Research Letters
Online Access:https://doi.org/10.1029/2024GL112817
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author Lei Chen
Jiayan Yang
Lixin Wu
author_facet Lei Chen
Jiayan Yang
Lixin Wu
author_sort Lei Chen
collection DOAJ
description Abstract The Luzon Strait Deep Overflow (LZDO) transports deep‐water masses from the Pacific Ocean (upstream) to the South China Sea (SCS, downstream), playing a vital role in shaping the hydrographic and biogeochemical structure and regulating abyssal circulation within the SCS. Recent studies suggest that the seasonal variability of LZDO transport is primarily wind‐driven; however, the specific mechanisms and key wind‐forcing areas remain unclear. In this study, we use numerical model experiments to demonstrate that the seasonal variability of the LZDO is driven by wind stress both within the downstream SCS and upstream Pacific Ocean. This finding contrasts with previous views that considered the LZDO hydraulically controlled at the Luzon Strait sill and thus influenced solely by the upstream Pacific Ocean forcing. Additionally, we identify that the LZDO is particularly sensitive to wind forcing in specific North Pacific regions where geostrophic contours connect to the Luzon Strait due to topographic effects.
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institution Kabale University
issn 0094-8276
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publishDate 2025-01-01
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series Geophysical Research Letters
spelling doaj-art-a2968b72cc064598a781d819b30f07e52025-01-20T13:05:57ZengWileyGeophysical Research Letters0094-82761944-80072025-01-01521n/an/a10.1029/2024GL112817Upstream and Downstream Wind‐Stress Forcing of Seasonal Variability of Luzon Strait Deep Overflow TransportLei Chen0Jiayan Yang1Lixin Wu2Frontier Science Center for Deep Ocean Multispheres and Earth System (FDOMES) and Physical Oceanography Laboratory Ocean University of China Qingdao ChinaDepartment of Physical Oceanography Woods Hole Oceanographic Institution Woods Hole MA USAFrontier Science Center for Deep Ocean Multispheres and Earth System (FDOMES) and Physical Oceanography Laboratory Ocean University of China Qingdao ChinaAbstract The Luzon Strait Deep Overflow (LZDO) transports deep‐water masses from the Pacific Ocean (upstream) to the South China Sea (SCS, downstream), playing a vital role in shaping the hydrographic and biogeochemical structure and regulating abyssal circulation within the SCS. Recent studies suggest that the seasonal variability of LZDO transport is primarily wind‐driven; however, the specific mechanisms and key wind‐forcing areas remain unclear. In this study, we use numerical model experiments to demonstrate that the seasonal variability of the LZDO is driven by wind stress both within the downstream SCS and upstream Pacific Ocean. This finding contrasts with previous views that considered the LZDO hydraulically controlled at the Luzon Strait sill and thus influenced solely by the upstream Pacific Ocean forcing. Additionally, we identify that the LZDO is particularly sensitive to wind forcing in specific North Pacific regions where geostrophic contours connect to the Luzon Strait due to topographic effects.https://doi.org/10.1029/2024GL112817
spellingShingle Lei Chen
Jiayan Yang
Lixin Wu
Upstream and Downstream Wind‐Stress Forcing of Seasonal Variability of Luzon Strait Deep Overflow Transport
Geophysical Research Letters
title Upstream and Downstream Wind‐Stress Forcing of Seasonal Variability of Luzon Strait Deep Overflow Transport
title_full Upstream and Downstream Wind‐Stress Forcing of Seasonal Variability of Luzon Strait Deep Overflow Transport
title_fullStr Upstream and Downstream Wind‐Stress Forcing of Seasonal Variability of Luzon Strait Deep Overflow Transport
title_full_unstemmed Upstream and Downstream Wind‐Stress Forcing of Seasonal Variability of Luzon Strait Deep Overflow Transport
title_short Upstream and Downstream Wind‐Stress Forcing of Seasonal Variability of Luzon Strait Deep Overflow Transport
title_sort upstream and downstream wind stress forcing of seasonal variability of luzon strait deep overflow transport
url https://doi.org/10.1029/2024GL112817
work_keys_str_mv AT leichen upstreamanddownstreamwindstressforcingofseasonalvariabilityofluzonstraitdeepoverflowtransport
AT jiayanyang upstreamanddownstreamwindstressforcingofseasonalvariabilityofluzonstraitdeepoverflowtransport
AT lixinwu upstreamanddownstreamwindstressforcingofseasonalvariabilityofluzonstraitdeepoverflowtransport