The Arctic sea ice extent change connected to Pacific decadal variability

<p>After an unprecedented retreat, the total Arctic sea ice cover for the post-2007 period is characterized by low extent and a remarkable increase in annual cycle amplitude. We have identified the leading role of spring Bering Sea ice in explaining the changes in the amplitude of the annual c...

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Main Authors: X.-Y. Yang, G. Wang, N. Keenlyside
Format: Article
Language:English
Published: Copernicus Publications 2020-02-01
Series:The Cryosphere
Online Access:https://www.the-cryosphere.net/14/693/2020/tc-14-693-2020.pdf
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spelling doaj-6e26e5aebf2a418fa7b379435312bd5c2020-11-25T02:11:03ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242020-02-011469370810.5194/tc-14-693-2020The Arctic sea ice extent change connected to Pacific decadal variabilityX.-Y. Yang0X.-Y. Yang1G. Wang2G. Wang3N. Keenlyside4N. Keenlyside5State Key Laboratory of Marine Environmental Science and College of Ocean and Earth Sciences, Xiamen University, Xiamen, ChinaSouthern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, ChinaDepartment of Atmospheric and Oceanic Sciences and Institute of Atmospheric Sciences, Fudan University, Shanghai, ChinaCMA-FDU Joint Laboratory of Marine Meteorology, Shanghai, ChinaGeophysical Institute, University of Bergen and Bjerknes Centre for Climate Research, Bergen, NorwayNansen Environmental and Remote Sensing Center, Bergen, Norway<p>After an unprecedented retreat, the total Arctic sea ice cover for the post-2007 period is characterized by low extent and a remarkable increase in annual cycle amplitude. We have identified the leading role of spring Bering Sea ice in explaining the changes in the amplitude of the annual cycle of total Arctic sea ice. In particular, these changes are related to the recent occurrence of multiyear variability in spring Bering Sea ice extent. This is due to the phase-locking of the North Pacific Gyre Oscillation (NPGO) and the Pacific Decadal Oscillation (PDO) after about 2007, with a correlation coefficient reaching <span class="inline-formula">−0.6</span>. Furthermore, there emerge notable changes in the sea level pressure and sea surface temperature patterns associated with the NPGO in the recent decade. After 2007, the NPGO is related to a quadrupole of sea level pressure (SLP) anomalies that is associated with the wind stress curl and Ekman pumping rate anomalies in the Bering deep basin; these account for the change in Bering Sea subsurface variability that contribute to the decadal oscillation of the spring Bering Sea ice extent.</p>https://www.the-cryosphere.net/14/693/2020/tc-14-693-2020.pdf
collection DOAJ
language English
format Article
sources DOAJ
author X.-Y. Yang
X.-Y. Yang
G. Wang
G. Wang
N. Keenlyside
N. Keenlyside
spellingShingle X.-Y. Yang
X.-Y. Yang
G. Wang
G. Wang
N. Keenlyside
N. Keenlyside
The Arctic sea ice extent change connected to Pacific decadal variability
The Cryosphere
author_facet X.-Y. Yang
X.-Y. Yang
G. Wang
G. Wang
N. Keenlyside
N. Keenlyside
author_sort X.-Y. Yang
title The Arctic sea ice extent change connected to Pacific decadal variability
title_short The Arctic sea ice extent change connected to Pacific decadal variability
title_full The Arctic sea ice extent change connected to Pacific decadal variability
title_fullStr The Arctic sea ice extent change connected to Pacific decadal variability
title_full_unstemmed The Arctic sea ice extent change connected to Pacific decadal variability
title_sort arctic sea ice extent change connected to pacific decadal variability
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2020-02-01
description <p>After an unprecedented retreat, the total Arctic sea ice cover for the post-2007 period is characterized by low extent and a remarkable increase in annual cycle amplitude. We have identified the leading role of spring Bering Sea ice in explaining the changes in the amplitude of the annual cycle of total Arctic sea ice. In particular, these changes are related to the recent occurrence of multiyear variability in spring Bering Sea ice extent. This is due to the phase-locking of the North Pacific Gyre Oscillation (NPGO) and the Pacific Decadal Oscillation (PDO) after about 2007, with a correlation coefficient reaching <span class="inline-formula">−0.6</span>. Furthermore, there emerge notable changes in the sea level pressure and sea surface temperature patterns associated with the NPGO in the recent decade. After 2007, the NPGO is related to a quadrupole of sea level pressure (SLP) anomalies that is associated with the wind stress curl and Ekman pumping rate anomalies in the Bering deep basin; these account for the change in Bering Sea subsurface variability that contribute to the decadal oscillation of the spring Bering Sea ice extent.</p>
url https://www.the-cryosphere.net/14/693/2020/tc-14-693-2020.pdf
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