Impacts of the Siberian High and Arctic Oscillation on the East Asia winter monsoon: Driving downwelling in the western Bering Sea

NOAA RUSALCA The relationships between the wind fields of the East Asia winter monsoon (EAWM), the Siberian High (SH), and the Arctic Oscillation (AO) were investigated using reanalysis products. The winter anomalies of the wind fields were systematically examined from the Bering Sea, the Sea of Okh...

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Main Authors: Wang, Jia, Bai, Xuezhi, Wang, Dongxiao, Wang, Daoru, Hu, Haoguo, Yang, Xiaoyi, 杨小怡
Format: Article in Journal/Newspaper
Language:English
Published: AQUAT ECOSYST HEALTH 2012
Subjects:
ICE
Online Access:http://dspace.xmu.edu.cn/handle/2288/87743
id ftxiamenuniv:oai:dspace.xmu.edu.cn:2288/87743
record_format openpolar
spelling ftxiamenuniv:oai:dspace.xmu.edu.cn:2288/87743 2023-05-15T13:15:07+02:00 Impacts of the Siberian High and Arctic Oscillation on the East Asia winter monsoon: Driving downwelling in the western Bering Sea Wang, Jia Bai, Xuezhi Wang, Dongxiao Wang, Daoru Hu, Haoguo Yang, Xiaoyi 杨小怡 2012 http://dspace.xmu.edu.cn/handle/2288/87743 en_US eng AQUAT ECOSYST HEALTH AQUATIC ECOSYSTEM HEALTH & MANAGEMENT, 2012,15(1):20-30 WOS:000301956600005 http://dspace.xmu.edu.cn/handle/2288/87743 http://dx.doi.org/10.1080/14634988.2012.648860 INTERANNUAL VARIABILITY LABRADOR SEA OCEAN MODEL ICE Article 2012 ftxiamenuniv 2020-07-21T11:42:21Z NOAA RUSALCA The relationships between the wind fields of the East Asia winter monsoon (EAWM), the Siberian High (SH), and the Arctic Oscillation (AO) were investigated using reanalysis products. The winter anomalies of the wind fields were systematically examined from the Bering Sea, the Sea of Okhotsk (SoO), the Sea of Japan (SOJ), the East China Sea (ECS), and all the way to the South China Sea (SCS). The sea-level pressure (SLP) difference between the SH and the Aleutian Low (AL) determines the intensity of the EAWM. Wind field anomalies are controlled directly by the SH and indirectly by the AO that has significant impacts on the SH and AL. It is found that +SH enhances the EAWM, while +AO reduces the intensity of the EAWM by reducing the SLP difference (gradient) between the SH and AL; vice versa for the -SH and -AO, respectively. The surface air temperature (SAT) anomalies caused by the +SH result in a significant cooling in the downstream regions and a warming in the upstream regions; vice versa for the negative phase of the SH. The +AO produces a large warming in northern Eurasian and a cooling in the Bering Sea. Furthermore, using a Coupled Ice-Ocean Model (CIOM), it is found that the EAWM can produce a downwelling and dense water formation along the Siberian coast in the western Bering Sea, and also a significant surface-to-bottom convection over the Bering shelf, forming the winter shelf water, which can survive the summer as the so-called cold pool. The cold pool in the Bering Sea has significant impacts on marine ecosystems and habitat including fisheries, which has much implication to other marginal seas of East Asia. Article in Journal/Newspaper aleutian low Arctic Bering Sea Labrador Sea RUSALCA Xiamen University Institutional Repository Arctic Bering Sea Okhotsk Bering Shelf ENVELOPE(-170.783,-170.783,60.128,60.128)
institution Open Polar
collection Xiamen University Institutional Repository
op_collection_id ftxiamenuniv
language English
topic INTERANNUAL VARIABILITY
LABRADOR SEA
OCEAN MODEL
ICE
spellingShingle INTERANNUAL VARIABILITY
LABRADOR SEA
OCEAN MODEL
ICE
Wang, Jia
Bai, Xuezhi
Wang, Dongxiao
Wang, Daoru
Hu, Haoguo
Yang, Xiaoyi
杨小怡
Impacts of the Siberian High and Arctic Oscillation on the East Asia winter monsoon: Driving downwelling in the western Bering Sea
topic_facet INTERANNUAL VARIABILITY
LABRADOR SEA
OCEAN MODEL
ICE
description NOAA RUSALCA The relationships between the wind fields of the East Asia winter monsoon (EAWM), the Siberian High (SH), and the Arctic Oscillation (AO) were investigated using reanalysis products. The winter anomalies of the wind fields were systematically examined from the Bering Sea, the Sea of Okhotsk (SoO), the Sea of Japan (SOJ), the East China Sea (ECS), and all the way to the South China Sea (SCS). The sea-level pressure (SLP) difference between the SH and the Aleutian Low (AL) determines the intensity of the EAWM. Wind field anomalies are controlled directly by the SH and indirectly by the AO that has significant impacts on the SH and AL. It is found that +SH enhances the EAWM, while +AO reduces the intensity of the EAWM by reducing the SLP difference (gradient) between the SH and AL; vice versa for the -SH and -AO, respectively. The surface air temperature (SAT) anomalies caused by the +SH result in a significant cooling in the downstream regions and a warming in the upstream regions; vice versa for the negative phase of the SH. The +AO produces a large warming in northern Eurasian and a cooling in the Bering Sea. Furthermore, using a Coupled Ice-Ocean Model (CIOM), it is found that the EAWM can produce a downwelling and dense water formation along the Siberian coast in the western Bering Sea, and also a significant surface-to-bottom convection over the Bering shelf, forming the winter shelf water, which can survive the summer as the so-called cold pool. The cold pool in the Bering Sea has significant impacts on marine ecosystems and habitat including fisheries, which has much implication to other marginal seas of East Asia.
format Article in Journal/Newspaper
author Wang, Jia
Bai, Xuezhi
Wang, Dongxiao
Wang, Daoru
Hu, Haoguo
Yang, Xiaoyi
杨小怡
author_facet Wang, Jia
Bai, Xuezhi
Wang, Dongxiao
Wang, Daoru
Hu, Haoguo
Yang, Xiaoyi
杨小怡
author_sort Wang, Jia
title Impacts of the Siberian High and Arctic Oscillation on the East Asia winter monsoon: Driving downwelling in the western Bering Sea
title_short Impacts of the Siberian High and Arctic Oscillation on the East Asia winter monsoon: Driving downwelling in the western Bering Sea
title_full Impacts of the Siberian High and Arctic Oscillation on the East Asia winter monsoon: Driving downwelling in the western Bering Sea
title_fullStr Impacts of the Siberian High and Arctic Oscillation on the East Asia winter monsoon: Driving downwelling in the western Bering Sea
title_full_unstemmed Impacts of the Siberian High and Arctic Oscillation on the East Asia winter monsoon: Driving downwelling in the western Bering Sea
title_sort impacts of the siberian high and arctic oscillation on the east asia winter monsoon: driving downwelling in the western bering sea
publisher AQUAT ECOSYST HEALTH
publishDate 2012
url http://dspace.xmu.edu.cn/handle/2288/87743
long_lat ENVELOPE(-170.783,-170.783,60.128,60.128)
geographic Arctic
Bering Sea
Okhotsk
Bering Shelf
geographic_facet Arctic
Bering Sea
Okhotsk
Bering Shelf
genre aleutian low
Arctic
Bering Sea
Labrador Sea
RUSALCA
genre_facet aleutian low
Arctic
Bering Sea
Labrador Sea
RUSALCA
op_source http://dx.doi.org/10.1080/14634988.2012.648860
op_relation AQUATIC ECOSYSTEM HEALTH & MANAGEMENT, 2012,15(1):20-30
WOS:000301956600005
http://dspace.xmu.edu.cn/handle/2288/87743
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