Impact of Kuroshio Extension dipole mode variability on the North Pacific storm track

An index of a large-scale Kuroshio Extension (KE) sea surface height dipole (KED) mode is constructed using satellite altimeter sea level anomaly observations from January 1993 to December 2015 based on previous work of the second author. It is found that the KED mode that undergoes a decadal variat...

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Main Authors: Jie Zhang, De-Hai Luo
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2017-09-01
Series:Atmospheric and Oceanic Science Letters
Subjects:
Online Access:http://dx.doi.org/10.1080/16742834.2017.1351864
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spelling doaj-df5e1f988fb348a8a91da4f6b64a55c02021-03-02T06:12:45ZengKeAi Communications Co., Ltd.Atmospheric and Oceanic Science Letters1674-28342376-61232017-09-0110538939610.1080/16742834.2017.13518641351864Impact of Kuroshio Extension dipole mode variability on the North Pacific storm trackJie Zhang0De-Hai Luo1Chinese Academy of SciencesChinese Academy of SciencesAn index of a large-scale Kuroshio Extension (KE) sea surface height dipole (KED) mode is constructed using satellite altimeter sea level anomaly observations from January 1993 to December 2015 based on previous work of the second author. It is found that the KED mode that undergoes a decadal variation from a negative phase (a positive-over-negative dipole, KED−) to a positive phase (a negative-over-positive dipole, KED+) can affect the variability of the oceanic SST front and the North Pacific storm track. The results show that the oceanic SST fronts in the north of the KE region and in the KE region — referred to as the NSST and KSST fronts, respectively — are closely correlated with the KED mode. In the NSST front region, the SST front is stronger for KED− than for KED+, and the opposite is the case in the KSST region. It is further revealed that the decadal phase transition of the KED mode can change the location and strength of the North Pacific storm track, with the North Pacific storm track being slightly weaker and moving more northwards as a whole during the KED− mode than during the KED+ mode. The westerly wind associated with the storm track on the downstream side of the KE region intensifies and shifts northwards under KED− compared to KED+. Furthermore, the transition of the KED mode gives rise to changes in the North Pacific storm track by changing the NSST and KSST fronts and meridional heat flux.http://dx.doi.org/10.1080/16742834.2017.1351864Kuroshio Extensionoceanic frontNorth Pacific storm track
collection DOAJ
language English
format Article
sources DOAJ
author Jie Zhang
De-Hai Luo
spellingShingle Jie Zhang
De-Hai Luo
Impact of Kuroshio Extension dipole mode variability on the North Pacific storm track
Atmospheric and Oceanic Science Letters
Kuroshio Extension
oceanic front
North Pacific storm track
author_facet Jie Zhang
De-Hai Luo
author_sort Jie Zhang
title Impact of Kuroshio Extension dipole mode variability on the North Pacific storm track
title_short Impact of Kuroshio Extension dipole mode variability on the North Pacific storm track
title_full Impact of Kuroshio Extension dipole mode variability on the North Pacific storm track
title_fullStr Impact of Kuroshio Extension dipole mode variability on the North Pacific storm track
title_full_unstemmed Impact of Kuroshio Extension dipole mode variability on the North Pacific storm track
title_sort impact of kuroshio extension dipole mode variability on the north pacific storm track
publisher KeAi Communications Co., Ltd.
series Atmospheric and Oceanic Science Letters
issn 1674-2834
2376-6123
publishDate 2017-09-01
description An index of a large-scale Kuroshio Extension (KE) sea surface height dipole (KED) mode is constructed using satellite altimeter sea level anomaly observations from January 1993 to December 2015 based on previous work of the second author. It is found that the KED mode that undergoes a decadal variation from a negative phase (a positive-over-negative dipole, KED−) to a positive phase (a negative-over-positive dipole, KED+) can affect the variability of the oceanic SST front and the North Pacific storm track. The results show that the oceanic SST fronts in the north of the KE region and in the KE region — referred to as the NSST and KSST fronts, respectively — are closely correlated with the KED mode. In the NSST front region, the SST front is stronger for KED− than for KED+, and the opposite is the case in the KSST region. It is further revealed that the decadal phase transition of the KED mode can change the location and strength of the North Pacific storm track, with the North Pacific storm track being slightly weaker and moving more northwards as a whole during the KED− mode than during the KED+ mode. The westerly wind associated with the storm track on the downstream side of the KE region intensifies and shifts northwards under KED− compared to KED+. Furthermore, the transition of the KED mode gives rise to changes in the North Pacific storm track by changing the NSST and KSST fronts and meridional heat flux.
topic Kuroshio Extension
oceanic front
North Pacific storm track
url http://dx.doi.org/10.1080/16742834.2017.1351864
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