Intrinsic and Wind-Driven Decadal Variability of the Kuroshio Extension in Altimeter Observations
In this work we use satellite altimeter observations to study the mechanism of decadal variability of the Kuroshio Extension (KE), with special attention on jet-eddy energy transfer, and on the relationship between the wind-driven sea surface height anomalies (SSHAs) and those directly driven by int...
Guardado en:
Autores principales: | , , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Frontiers Media S.A.
2021
|
Materias: | |
Acceso en línea: | https://doaj.org/article/d3cd0554b42e422d9fbf1b8bf2f9b30d |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
id |
oai:doaj.org-article:d3cd0554b42e422d9fbf1b8bf2f9b30d |
---|---|
record_format |
dspace |
spelling |
oai:doaj.org-article:d3cd0554b42e422d9fbf1b8bf2f9b30d2021-11-22T06:35:27ZIntrinsic and Wind-Driven Decadal Variability of the Kuroshio Extension in Altimeter Observations2296-774510.3389/fmars.2021.766226https://doaj.org/article/d3cd0554b42e422d9fbf1b8bf2f9b30d2021-11-01T00:00:00Zhttps://www.frontiersin.org/articles/10.3389/fmars.2021.766226/fullhttps://doaj.org/toc/2296-7745In this work we use satellite altimeter observations to study the mechanism of decadal variability of the Kuroshio Extension (KE), with special attention on jet-eddy energy transfer, and on the relationship between the wind-driven sea surface height anomalies (SSHAs) and those directly driven by intrinsic oceanic processes including jet and eddies. It is shown that energy feedback between the jet and mesoscale eddies can maintain the decadal oscillation of the KE. The wind-driven SSHAs are broad-scale and very weak compared to the intrinsic variability. Physically they can potentially trigger delayed responses of the latter by modulating vorticity advection from upstream but the statistical significance is low. KE perturbations resulting from the intrinsic variability, on the other hand, could feedback onto the wind-driven SSHAs by inducing anomalous basin-scale wind stress. The KE jet is thus an integrated system involving the jet and the eddies, possibly feeding back to, and paced by, wind stress anomalies.Guidi ZhouGuidi ZhouZhuhua LiZhuhua LiXuhua ChengXuhua ChengFrontiers Media S.A.articleKuroshio Extensionmesoscale eddyRossby wavewind stress forcingdecadal variabilityScienceQGeneral. Including nature conservation, geographical distributionQH1-199.5ENFrontiers in Marine Science, Vol 8 (2021) |
institution |
DOAJ |
collection |
DOAJ |
language |
EN |
topic |
Kuroshio Extension mesoscale eddy Rossby wave wind stress forcing decadal variability Science Q General. Including nature conservation, geographical distribution QH1-199.5 |
spellingShingle |
Kuroshio Extension mesoscale eddy Rossby wave wind stress forcing decadal variability Science Q General. Including nature conservation, geographical distribution QH1-199.5 Guidi Zhou Guidi Zhou Zhuhua Li Zhuhua Li Xuhua Cheng Xuhua Cheng Intrinsic and Wind-Driven Decadal Variability of the Kuroshio Extension in Altimeter Observations |
description |
In this work we use satellite altimeter observations to study the mechanism of decadal variability of the Kuroshio Extension (KE), with special attention on jet-eddy energy transfer, and on the relationship between the wind-driven sea surface height anomalies (SSHAs) and those directly driven by intrinsic oceanic processes including jet and eddies. It is shown that energy feedback between the jet and mesoscale eddies can maintain the decadal oscillation of the KE. The wind-driven SSHAs are broad-scale and very weak compared to the intrinsic variability. Physically they can potentially trigger delayed responses of the latter by modulating vorticity advection from upstream but the statistical significance is low. KE perturbations resulting from the intrinsic variability, on the other hand, could feedback onto the wind-driven SSHAs by inducing anomalous basin-scale wind stress. The KE jet is thus an integrated system involving the jet and the eddies, possibly feeding back to, and paced by, wind stress anomalies. |
format |
article |
author |
Guidi Zhou Guidi Zhou Zhuhua Li Zhuhua Li Xuhua Cheng Xuhua Cheng |
author_facet |
Guidi Zhou Guidi Zhou Zhuhua Li Zhuhua Li Xuhua Cheng Xuhua Cheng |
author_sort |
Guidi Zhou |
title |
Intrinsic and Wind-Driven Decadal Variability of the Kuroshio Extension in Altimeter Observations |
title_short |
Intrinsic and Wind-Driven Decadal Variability of the Kuroshio Extension in Altimeter Observations |
title_full |
Intrinsic and Wind-Driven Decadal Variability of the Kuroshio Extension in Altimeter Observations |
title_fullStr |
Intrinsic and Wind-Driven Decadal Variability of the Kuroshio Extension in Altimeter Observations |
title_full_unstemmed |
Intrinsic and Wind-Driven Decadal Variability of the Kuroshio Extension in Altimeter Observations |
title_sort |
intrinsic and wind-driven decadal variability of the kuroshio extension in altimeter observations |
publisher |
Frontiers Media S.A. |
publishDate |
2021 |
url |
https://doaj.org/article/d3cd0554b42e422d9fbf1b8bf2f9b30d |
work_keys_str_mv |
AT guidizhou intrinsicandwinddrivendecadalvariabilityofthekuroshioextensioninaltimeterobservations AT guidizhou intrinsicandwinddrivendecadalvariabilityofthekuroshioextensioninaltimeterobservations AT zhuhuali intrinsicandwinddrivendecadalvariabilityofthekuroshioextensioninaltimeterobservations AT zhuhuali intrinsicandwinddrivendecadalvariabilityofthekuroshioextensioninaltimeterobservations AT xuhuacheng intrinsicandwinddrivendecadalvariabilityofthekuroshioextensioninaltimeterobservations AT xuhuacheng intrinsicandwinddrivendecadalvariabilityofthekuroshioextensioninaltimeterobservations |
_version_ |
1718418129375199232 |