Propagation of planetary-scale zonal mean wind anomalies and polar oscillations
Global atmospheric variables can be physically decomposed into four components: (1) the zonal time averaged climate symmetric component, (2) the time averaged climate asymmetric, (3) the zonal-mean transient symmetric anomaly, and (4) the transient asymmetric anomaly. This study analyzes the relatio...
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科学通报 英文版
2012
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ftpekinguniv:oai:localhost:20.500.11897/148402 2023-05-15T13:34:56+02:00 Propagation of planetary-scale zonal mean wind anomalies and polar oscillations Qian WeiHong Liang HaoYuan Qian, WH (reprint author), Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China. Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China. 2012 https://hdl.handle.net/20.500.11897/148402 https://doi.org/10.1007/s11434-012-5168-1 en eng 科学通报 英文版 CHINESE SCIENCE BULLETIN.2012,57,(20),2606-2614. 873432 1001-6538 http://hdl.handle.net/20.500.11897/148402 doi:10.1007/s11434-012-5168-1 WOS:000305916000015 SCI physical decomposition El Nino-Southern Oscillation Arctic Oscillation Antarctic Oscillation planetary scale intra-seasonal oscillations TEMPERATURE CIRCULATION PACIFIC Journal 2012 ftpekinguniv https://doi.org/20.500.11897/148402 https://doi.org/10.1007/s11434-012-5168-1 2021-08-01T07:58:26Z Global atmospheric variables can be physically decomposed into four components: (1) the zonal time averaged climate symmetric component, (2) the time averaged climate asymmetric, (3) the zonal-mean transient symmetric anomaly, and (4) the transient asymmetric anomaly. This study analyzes the relationships between the intra-seasonal and inter-annual variability of planetary scale decomposed zonal and meridional winds in the tropopause, and oscillations such as those from the El Nino-Southern Oscillation (ENSO), the Arctic Oscillation (AO) and the Antarctic Oscillation (AAO). The tropical inter-annual zonal mean wind anomalies in the tropopause are linked with the ENSO cycle and can propagate into the subtropics, mid-latitudes, and polar front regions via abnormal meridional vertical cells. Similarly, tropical intra-seasonal (40-60-d) zonal wind anomalies can reach the subtropics and mid-latitudes. The polar intra-seasonal zonal wind anomalies in the tropopause can propagate toward high-latitude areas. Thus, the AO and the AAO are the result of the interaction and propagation of these planetary scale zonal wind anomalies. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000305916000015&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Multidisciplinary Sciences SCI(E) 6 ARTICLE 20 2606-2614 57 Journal/Newspaper Antarc* Antarctic Arctic Peking University Institutional Repository (PKU IR) Antarctic Arctic Pacific The Antarctic Chinese Science Bulletin 57 20 2606 2614 |
institution |
Open Polar |
collection |
Peking University Institutional Repository (PKU IR) |
op_collection_id |
ftpekinguniv |
language |
English |
topic |
physical decomposition El Nino-Southern Oscillation Arctic Oscillation Antarctic Oscillation planetary scale intra-seasonal oscillations TEMPERATURE CIRCULATION PACIFIC |
spellingShingle |
physical decomposition El Nino-Southern Oscillation Arctic Oscillation Antarctic Oscillation planetary scale intra-seasonal oscillations TEMPERATURE CIRCULATION PACIFIC Qian WeiHong Liang HaoYuan Propagation of planetary-scale zonal mean wind anomalies and polar oscillations |
topic_facet |
physical decomposition El Nino-Southern Oscillation Arctic Oscillation Antarctic Oscillation planetary scale intra-seasonal oscillations TEMPERATURE CIRCULATION PACIFIC |
description |
Global atmospheric variables can be physically decomposed into four components: (1) the zonal time averaged climate symmetric component, (2) the time averaged climate asymmetric, (3) the zonal-mean transient symmetric anomaly, and (4) the transient asymmetric anomaly. This study analyzes the relationships between the intra-seasonal and inter-annual variability of planetary scale decomposed zonal and meridional winds in the tropopause, and oscillations such as those from the El Nino-Southern Oscillation (ENSO), the Arctic Oscillation (AO) and the Antarctic Oscillation (AAO). The tropical inter-annual zonal mean wind anomalies in the tropopause are linked with the ENSO cycle and can propagate into the subtropics, mid-latitudes, and polar front regions via abnormal meridional vertical cells. Similarly, tropical intra-seasonal (40-60-d) zonal wind anomalies can reach the subtropics and mid-latitudes. The polar intra-seasonal zonal wind anomalies in the tropopause can propagate toward high-latitude areas. Thus, the AO and the AAO are the result of the interaction and propagation of these planetary scale zonal wind anomalies. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000305916000015&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Multidisciplinary Sciences SCI(E) 6 ARTICLE 20 2606-2614 57 |
author2 |
Qian, WH (reprint author), Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China. Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China. |
format |
Journal/Newspaper |
author |
Qian WeiHong Liang HaoYuan |
author_facet |
Qian WeiHong Liang HaoYuan |
author_sort |
Qian WeiHong |
title |
Propagation of planetary-scale zonal mean wind anomalies and polar oscillations |
title_short |
Propagation of planetary-scale zonal mean wind anomalies and polar oscillations |
title_full |
Propagation of planetary-scale zonal mean wind anomalies and polar oscillations |
title_fullStr |
Propagation of planetary-scale zonal mean wind anomalies and polar oscillations |
title_full_unstemmed |
Propagation of planetary-scale zonal mean wind anomalies and polar oscillations |
title_sort |
propagation of planetary-scale zonal mean wind anomalies and polar oscillations |
publisher |
科学通报 英文版 |
publishDate |
2012 |
url |
https://hdl.handle.net/20.500.11897/148402 https://doi.org/10.1007/s11434-012-5168-1 |
geographic |
Antarctic Arctic Pacific The Antarctic |
geographic_facet |
Antarctic Arctic Pacific The Antarctic |
genre |
Antarc* Antarctic Arctic |
genre_facet |
Antarc* Antarctic Arctic |
op_source |
SCI |
op_relation |
CHINESE SCIENCE BULLETIN.2012,57,(20),2606-2614. 873432 1001-6538 http://hdl.handle.net/20.500.11897/148402 doi:10.1007/s11434-012-5168-1 WOS:000305916000015 |
op_doi |
https://doi.org/20.500.11897/148402 https://doi.org/10.1007/s11434-012-5168-1 |
container_title |
Chinese Science Bulletin |
container_volume |
57 |
container_issue |
20 |
container_start_page |
2606 |
op_container_end_page |
2614 |
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1766059234717335552 |