Synoptic-scale variability in the Beaufort High and spring ice opening in the Beaufort Sea

This study examines the role of synoptic-scale variability in the Beaufort High in spring ice opening in the Beaufort Sea using data over the 2000–2019 period. A few days before ice opening in spring, the Beaufort High begins to strengthen, deform, and shift eastward from the Chukchi Sea to the west...

Full description

Bibliographic Details
Main Authors: Yingqi Huang, Xuezhi Bai, Hengling Leng
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-07-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2022.929209/full
_version_ 1828777511686766592
author Yingqi Huang
Yingqi Huang
Xuezhi Bai
Xuezhi Bai
Hengling Leng
author_facet Yingqi Huang
Yingqi Huang
Xuezhi Bai
Xuezhi Bai
Hengling Leng
author_sort Yingqi Huang
collection DOAJ
description This study examines the role of synoptic-scale variability in the Beaufort High in spring ice opening in the Beaufort Sea using data over the 2000–2019 period. A few days before ice opening in spring, the Beaufort High begins to strengthen, deform, and shift eastward from the Chukchi Sea to the western Canadian Arctic Archipelago due to warming in eastern Siberia, and the Aleutian Low is also enhanced. The pressure gradient between the Aleutian Low and the Beaufort High increases rapidly, promoting strong southeasterly winds. As the Beaufort High shifts eastward, the anticyclonic sea ice circulation in the Beaufort Sea tends to be an asymmetrical gyre; as a result, sea ice in the eastern Beaufort Sea is exported toward the western Beaufort Sea without supplementation from the north. Sea ice volume budget analysis indicates that when southeasterly winds are prevailing, wind-forced ice advection and divergence dominate the ice opening in the southeastern Beaufort Sea. Although both the basal and lateral melting are promoted during the ice opening, their contributions to the reduction of ice volume are negligible.
first_indexed 2024-12-11T16:22:18Z
format Article
id doaj.art-da28f49699864a8685888c603b4ac16e
institution Directory Open Access Journal
issn 2296-7745
language English
last_indexed 2024-12-11T16:22:18Z
publishDate 2022-07-01
publisher Frontiers Media S.A.
record_format Article
series Frontiers in Marine Science
spelling doaj.art-da28f49699864a8685888c603b4ac16e2022-12-22T00:58:49ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452022-07-01910.3389/fmars.2022.929209929209Synoptic-scale variability in the Beaufort High and spring ice opening in the Beaufort SeaYingqi Huang0Yingqi Huang1Xuezhi Bai2Xuezhi Bai3Hengling Leng4Key Laboratory of Marine Hazards Forecasting, Ministry of Natural Resources, Hohai University, Nanjing, ChinaCollege of Oceanography, Hohai University, Nanjing, ChinaKey Laboratory of Marine Hazards Forecasting, Ministry of Natural Resources, Hohai University, Nanjing, ChinaCollege of Oceanography, Hohai University, Nanjing, ChinaState Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, ChinaThis study examines the role of synoptic-scale variability in the Beaufort High in spring ice opening in the Beaufort Sea using data over the 2000–2019 period. A few days before ice opening in spring, the Beaufort High begins to strengthen, deform, and shift eastward from the Chukchi Sea to the western Canadian Arctic Archipelago due to warming in eastern Siberia, and the Aleutian Low is also enhanced. The pressure gradient between the Aleutian Low and the Beaufort High increases rapidly, promoting strong southeasterly winds. As the Beaufort High shifts eastward, the anticyclonic sea ice circulation in the Beaufort Sea tends to be an asymmetrical gyre; as a result, sea ice in the eastern Beaufort Sea is exported toward the western Beaufort Sea without supplementation from the north. Sea ice volume budget analysis indicates that when southeasterly winds are prevailing, wind-forced ice advection and divergence dominate the ice opening in the southeastern Beaufort Sea. Although both the basal and lateral melting are promoted during the ice opening, their contributions to the reduction of ice volume are negligible.https://www.frontiersin.org/articles/10.3389/fmars.2022.929209/fullBeaufort HighSpring ice openingBeaufort Seasoutheasterly windssynoptic-scale variability
spellingShingle Yingqi Huang
Yingqi Huang
Xuezhi Bai
Xuezhi Bai
Hengling Leng
Synoptic-scale variability in the Beaufort High and spring ice opening in the Beaufort Sea
Frontiers in Marine Science
Beaufort High
Spring ice opening
Beaufort Sea
southeasterly winds
synoptic-scale variability
title Synoptic-scale variability in the Beaufort High and spring ice opening in the Beaufort Sea
title_full Synoptic-scale variability in the Beaufort High and spring ice opening in the Beaufort Sea
title_fullStr Synoptic-scale variability in the Beaufort High and spring ice opening in the Beaufort Sea
title_full_unstemmed Synoptic-scale variability in the Beaufort High and spring ice opening in the Beaufort Sea
title_short Synoptic-scale variability in the Beaufort High and spring ice opening in the Beaufort Sea
title_sort synoptic scale variability in the beaufort high and spring ice opening in the beaufort sea
topic Beaufort High
Spring ice opening
Beaufort Sea
southeasterly winds
synoptic-scale variability
url https://www.frontiersin.org/articles/10.3389/fmars.2022.929209/full
work_keys_str_mv AT yingqihuang synopticscalevariabilityinthebeauforthighandspringiceopeninginthebeaufortsea
AT yingqihuang synopticscalevariabilityinthebeauforthighandspringiceopeninginthebeaufortsea
AT xuezhibai synopticscalevariabilityinthebeauforthighandspringiceopeninginthebeaufortsea
AT xuezhibai synopticscalevariabilityinthebeauforthighandspringiceopeninginthebeaufortsea
AT henglingleng synopticscalevariabilityinthebeauforthighandspringiceopeninginthebeaufortsea