An Atlantic-driven rapid circulation change in the North Pacific Ocean during the late 1990s

Abstract Interbasin interactions have been increasingly emphasized in recent years due to their roles in shaping climate trends and the global warming hiatus in the northern hemisphere. The profound influence from the North Atlantic on the Tropical Pacific has been a primary focus. In this study, we...

Full description

Bibliographic Details
Main Authors: Chau-Ron Wu, Yong-Fu Lin, You-Lin Wang, Noel Keenlyside, Jin-Yi Yu
Format: Article
Language:English
Published: Nature Publishing Group 2019-10-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-019-51076-1
id doaj-005e8d803df642db9dd58f9f8d89fa34
record_format Article
spelling doaj-005e8d803df642db9dd58f9f8d89fa342020-12-08T06:58:35ZengNature Publishing GroupScientific Reports2045-23222019-10-01911810.1038/s41598-019-51076-1An Atlantic-driven rapid circulation change in the North Pacific Ocean during the late 1990sChau-Ron Wu0Yong-Fu Lin1You-Lin Wang2Noel Keenlyside3Jin-Yi Yu4Department of Earth Sciences, National Taiwan Normal UniversityDepartment of Earth Sciences, National Taiwan Normal UniversityDepartment of Earth Sciences, National Taiwan Normal UniversityGeophysical Institute, University of Bergen and Bjerknes Centre for Climate ResearchDepartment of Earth System Science, University of California at IrvineAbstract Interbasin interactions have been increasingly emphasized in recent years due to their roles in shaping climate trends and the global warming hiatus in the northern hemisphere. The profound influence from the North Atlantic on the Tropical Pacific has been a primary focus. In this study, we conducted observational analyses and numerical modeling experiments to show that the North Atlantic has also strongly influenced the Extratropical North Pacific. A rapid and synchronous change in the atmospheric and oceanic circulations was observed in the North Pacific during the late 1990s. The change was driven by the transbasin influence from the Atlantic Ocean. During the positive phase of the Atlantic Multidecadal Oscillation (AMO) since the 1990s, the anomalously warm North Atlantic triggers a series of zonally symmetric and asymmetric transbasin teleconnections involving the Inter-tropical Convergence Zone (ITCZ), Walker and Hadley circulations, and Rossby wave propagation that lead to a decrease in wind stress curls over the Pacific subtropics, resulting in an abrupt weakening in the North Pacific subtropical gyre (NPSG) and the Kuroshio Current.https://doi.org/10.1038/s41598-019-51076-1
collection DOAJ
language English
format Article
sources DOAJ
author Chau-Ron Wu
Yong-Fu Lin
You-Lin Wang
Noel Keenlyside
Jin-Yi Yu
spellingShingle Chau-Ron Wu
Yong-Fu Lin
You-Lin Wang
Noel Keenlyside
Jin-Yi Yu
An Atlantic-driven rapid circulation change in the North Pacific Ocean during the late 1990s
Scientific Reports
author_facet Chau-Ron Wu
Yong-Fu Lin
You-Lin Wang
Noel Keenlyside
Jin-Yi Yu
author_sort Chau-Ron Wu
title An Atlantic-driven rapid circulation change in the North Pacific Ocean during the late 1990s
title_short An Atlantic-driven rapid circulation change in the North Pacific Ocean during the late 1990s
title_full An Atlantic-driven rapid circulation change in the North Pacific Ocean during the late 1990s
title_fullStr An Atlantic-driven rapid circulation change in the North Pacific Ocean during the late 1990s
title_full_unstemmed An Atlantic-driven rapid circulation change in the North Pacific Ocean during the late 1990s
title_sort atlantic-driven rapid circulation change in the north pacific ocean during the late 1990s
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2019-10-01
description Abstract Interbasin interactions have been increasingly emphasized in recent years due to their roles in shaping climate trends and the global warming hiatus in the northern hemisphere. The profound influence from the North Atlantic on the Tropical Pacific has been a primary focus. In this study, we conducted observational analyses and numerical modeling experiments to show that the North Atlantic has also strongly influenced the Extratropical North Pacific. A rapid and synchronous change in the atmospheric and oceanic circulations was observed in the North Pacific during the late 1990s. The change was driven by the transbasin influence from the Atlantic Ocean. During the positive phase of the Atlantic Multidecadal Oscillation (AMO) since the 1990s, the anomalously warm North Atlantic triggers a series of zonally symmetric and asymmetric transbasin teleconnections involving the Inter-tropical Convergence Zone (ITCZ), Walker and Hadley circulations, and Rossby wave propagation that lead to a decrease in wind stress curls over the Pacific subtropics, resulting in an abrupt weakening in the North Pacific subtropical gyre (NPSG) and the Kuroshio Current.
url https://doi.org/10.1038/s41598-019-51076-1
work_keys_str_mv AT chauronwu anatlanticdrivenrapidcirculationchangeinthenorthpacificoceanduringthelate1990s
AT yongfulin anatlanticdrivenrapidcirculationchangeinthenorthpacificoceanduringthelate1990s
AT youlinwang anatlanticdrivenrapidcirculationchangeinthenorthpacificoceanduringthelate1990s
AT noelkeenlyside anatlanticdrivenrapidcirculationchangeinthenorthpacificoceanduringthelate1990s
AT jinyiyu anatlanticdrivenrapidcirculationchangeinthenorthpacificoceanduringthelate1990s
AT chauronwu atlanticdrivenrapidcirculationchangeinthenorthpacificoceanduringthelate1990s
AT yongfulin atlanticdrivenrapidcirculationchangeinthenorthpacificoceanduringthelate1990s
AT youlinwang atlanticdrivenrapidcirculationchangeinthenorthpacificoceanduringthelate1990s
AT noelkeenlyside atlanticdrivenrapidcirculationchangeinthenorthpacificoceanduringthelate1990s
AT jinyiyu atlanticdrivenrapidcirculationchangeinthenorthpacificoceanduringthelate1990s
_version_ 1724391242677092352