Further exploration on causes of temperature anomalies associated with the abnormal northern annular mode

This article concerns the temperature anomalies during the high index phase of the northern annual mode for the wintertime from January to March. The response of the zonal and meridional winds and the temperature advection caused by the anomalous horizontal wind are investigated. The results show th...

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Published in:Science Bulletin
Main Authors: Suo LingLing, Tan BenKui, Huang JiaYou
Other Authors: Tan, BK (reprint author), Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China., Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China.
Format: Journal/Newspaper
Language:English
Published: 科学通报 英文版 2009
Subjects:
Online Access:https://hdl.handle.net/20.500.11897/148817
https://doi.org/10.1007/s11434-009-0045-2
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author Suo LingLing
Tan BenKui
Huang JiaYou
author2 Tan, BK (reprint author), Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China.
Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China.
author_facet Suo LingLing
Tan BenKui
Huang JiaYou
author_sort Suo LingLing
collection Peking University Institutional Repository (PKU IR)
container_issue 12
container_start_page 2101
container_title Science Bulletin
container_volume 54
description This article concerns the temperature anomalies during the high index phase of the northern annual mode for the wintertime from January to March. The response of the zonal and meridional winds and the temperature advection caused by the anomalous horizontal wind are investigated. The results show that both the zonal and meridional winds experience strong anomalies and the temperature advection induced by both the anomalous zonal and meridional winds is responsible for the temperature anomalies associated with the high index northern annual mode. The temperature advection induced by the anomalous zonal wind contributes dominantly to the cooling in the Atlantic and the Bering Sea while the temperature advection induced by the anomalous merional wind contributes dominantly the warming in the United States of America and the cooling in southern Europe and Canada. The superposed influences caused the obvious warming in north Eurasia. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000267145500018&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Multidisciplinary Sciences SCI(E) 4 ARTICLE 12 2101-2106 54
format Journal/Newspaper
genre Arctic
Bering Sea
genre_facet Arctic
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geographic Arctic
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op_relation CHINESE SCIENCE BULLETIN.2009,54,(12),2101-2106.
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spelling ftpekinguniv:oai:localhost:20.500.11897/148817 2025-01-16T20:37:59+00:00 Further exploration on causes of temperature anomalies associated with the abnormal northern annular mode Suo LingLing Tan BenKui Huang JiaYou Tan, BK (reprint author), Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China. Peking Univ, Sch Phys, Dept Atmospher Sci, Beijing 100871, Peoples R China. 2009 https://hdl.handle.net/20.500.11897/148817 https://doi.org/10.1007/s11434-009-0045-2 en eng 科学通报 英文版 CHINESE SCIENCE BULLETIN.2009,54,(12),2101-2106. 937513 1001-6538 http://hdl.handle.net/20.500.11897/148817 doi:10.1007/s11434-009-0045-2 WOS:000267145500018 SCI northern annular mode Arctic Oscillation temperature advection air temperature anomaly abnormal wind FREQUENCY DIPOLE MODES CLIMATE VARIABILITY PART I DYNAMICS Journal 2009 ftpekinguniv https://doi.org/20.500.11897/148817 https://doi.org/10.1007/s11434-009-0045-2 2021-08-01T07:58:40Z This article concerns the temperature anomalies during the high index phase of the northern annual mode for the wintertime from January to March. The response of the zonal and meridional winds and the temperature advection caused by the anomalous horizontal wind are investigated. The results show that both the zonal and meridional winds experience strong anomalies and the temperature advection induced by both the anomalous zonal and meridional winds is responsible for the temperature anomalies associated with the high index northern annual mode. The temperature advection induced by the anomalous zonal wind contributes dominantly to the cooling in the Atlantic and the Bering Sea while the temperature advection induced by the anomalous merional wind contributes dominantly the warming in the United States of America and the cooling in southern Europe and Canada. The superposed influences caused the obvious warming in north Eurasia. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000267145500018&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Multidisciplinary Sciences SCI(E) 4 ARTICLE 12 2101-2106 54 Journal/Newspaper Arctic Bering Sea Peking University Institutional Repository (PKU IR) Arctic Bering Sea Canada Science Bulletin 54 12 2101 2106
spellingShingle northern annular mode
Arctic Oscillation
temperature advection
air temperature anomaly
abnormal wind
FREQUENCY DIPOLE MODES
CLIMATE VARIABILITY
PART I
DYNAMICS
Suo LingLing
Tan BenKui
Huang JiaYou
Further exploration on causes of temperature anomalies associated with the abnormal northern annular mode
title Further exploration on causes of temperature anomalies associated with the abnormal northern annular mode
title_full Further exploration on causes of temperature anomalies associated with the abnormal northern annular mode
title_fullStr Further exploration on causes of temperature anomalies associated with the abnormal northern annular mode
title_full_unstemmed Further exploration on causes of temperature anomalies associated with the abnormal northern annular mode
title_short Further exploration on causes of temperature anomalies associated with the abnormal northern annular mode
title_sort further exploration on causes of temperature anomalies associated with the abnormal northern annular mode
topic northern annular mode
Arctic Oscillation
temperature advection
air temperature anomaly
abnormal wind
FREQUENCY DIPOLE MODES
CLIMATE VARIABILITY
PART I
DYNAMICS
topic_facet northern annular mode
Arctic Oscillation
temperature advection
air temperature anomaly
abnormal wind
FREQUENCY DIPOLE MODES
CLIMATE VARIABILITY
PART I
DYNAMICS
url https://hdl.handle.net/20.500.11897/148817
https://doi.org/10.1007/s11434-009-0045-2