北半球大气遥相关型与区域尺度大气扰动

北极涛动(AO)、北大西洋涛动(NAO)和太平洋—北美型(PNA)等北半球大气遥相关型,可以用大气位势高度的物理分解扰动分量解释.结果发现,AO反映的是北极地区行星尺度纬圈平均扰动分量的变化,PNA与持续性天气尺度扰动分量相联系,NAO是行星尺度纬圈平均扰动与天气尺度扰动共同作用的结果.对行星尺度纬圈平均扰动分量和天气尺度扰动分量用旋转经验正交函数(REOF)展开,不但可以证实人们已经命名的区域性大气涛动,还新发现了北极地区的两对偶极涛动、欧亚涛动(EAO)和"大西洋—欧亚型"(AEA)波列.这些涛动连接了相邻地区的异常天气和异常气候. Atmospheric teleco...

Full description

Bibliographic Details
Main Authors: 钱维宏, 梁浩原
Other Authors: 北京大学大气海洋科学系
Format: Journal/Newspaper
Language:Chinese
Published: 地球物理学报 2012
Subjects:
Online Access:https://hdl.handle.net/20.500.11897/177588
https://doi.org/10.6038/j.issn.0001-5733.2012.05.003
id ftpekinguniv:oai:localhost:20.500.11897/177588
record_format openpolar
spelling ftpekinguniv:oai:localhost:20.500.11897/177588 2023-05-15T14:58:15+02:00 北半球大气遥相关型与区域尺度大气扰动 Atmospheric teleconnections and regional-scale atmospheric anomalies over the Northern Hemisphere 钱维宏 梁浩原 北京大学大气海洋科学系 2012 https://hdl.handle.net/20.500.11897/177588 https://doi.org/10.6038/j.issn.0001-5733.2012.05.003 zh chi 地球物理学报 地球物理学报.2012,(05),1449-1461. 878498 0001-5733 http://hdl.handle.net/20.500.11897/177588 doi:10.6038/j.issn.0001-5733.2012.05.003 WOS:000304734300003 万方 知网 SCI 大气遥相关 物理分解 北极涛动 北大西洋涛动 太平洋—北美遥相关型 Atmospheric teleconnections Physical decomposition Arctic Oscillation North Atlantic Oscillation Pacific-North American teleconnection pattern Journal 2012 ftpekinguniv https://doi.org/20.500.11897/177588 https://doi.org/10.6038/j.issn.0001-5733.2012.05.003 2021-08-01T08:14:42Z 北极涛动(AO)、北大西洋涛动(NAO)和太平洋—北美型(PNA)等北半球大气遥相关型,可以用大气位势高度的物理分解扰动分量解释.结果发现,AO反映的是北极地区行星尺度纬圈平均扰动分量的变化,PNA与持续性天气尺度扰动分量相联系,NAO是行星尺度纬圈平均扰动与天气尺度扰动共同作用的结果.对行星尺度纬圈平均扰动分量和天气尺度扰动分量用旋转经验正交函数(REOF)展开,不但可以证实人们已经命名的区域性大气涛动,还新发现了北极地区的两对偶极涛动、欧亚涛动(EAO)和"大西洋—欧亚型"(AEA)波列.这些涛动连接了相邻地区的异常天气和异常气候. Atmospheric teleconnections in the Northern Hemisphere such as Arctic Oscillation (AO), North Atlantic Oscillation (NAO) and Pacific-North American (PNA) teleconnection can be explained by the physical decomposition of geopotential height. The result shows that the AO reflects planetary-scale zonal-mean anomalies in the Arctic region; the PNA results from persistent regional-scale atmospheric anomalies; NAO is a combined result of both planetary-scale zonal-mean and regional-scale anomalies. The rotated empirical orthogonal function (REOF) of planetary-scale zonal-mean and regional-scale anomalies not only confirms the already known regional oscillations and wave trains, but also discovers new patterns, such as "twin dipole oscillations" in the Arctic region, Euro-Asia Oscillation (EAO) and Atlantic-Euro-Asia (AEA) wave-train pattern. These oscillations or wave trains are linked to adjacent regional weather anomalies and climate anomalies. SCI(E) 中文核心期刊要目总览(PKU) 中国科技核心期刊(ISTIC) 中国科学引文数据库(CSCD) 0 05 1449-1461 55 Journal/Newspaper Arctic North Atlantic North Atlantic oscillation Peking University Institutional Repository (PKU IR) Arctic Pacific
institution Open Polar
collection Peking University Institutional Repository (PKU IR)
op_collection_id ftpekinguniv
language Chinese
topic 大气遥相关
物理分解
北极涛动
北大西洋涛动
太平洋—北美遥相关型
Atmospheric teleconnections
Physical decomposition
Arctic Oscillation
North Atlantic Oscillation
Pacific-North American teleconnection pattern
spellingShingle 大气遥相关
物理分解
北极涛动
北大西洋涛动
太平洋—北美遥相关型
Atmospheric teleconnections
Physical decomposition
Arctic Oscillation
North Atlantic Oscillation
Pacific-North American teleconnection pattern
钱维宏
梁浩原
北半球大气遥相关型与区域尺度大气扰动
topic_facet 大气遥相关
物理分解
北极涛动
北大西洋涛动
太平洋—北美遥相关型
Atmospheric teleconnections
Physical decomposition
Arctic Oscillation
North Atlantic Oscillation
Pacific-North American teleconnection pattern
description 北极涛动(AO)、北大西洋涛动(NAO)和太平洋—北美型(PNA)等北半球大气遥相关型,可以用大气位势高度的物理分解扰动分量解释.结果发现,AO反映的是北极地区行星尺度纬圈平均扰动分量的变化,PNA与持续性天气尺度扰动分量相联系,NAO是行星尺度纬圈平均扰动与天气尺度扰动共同作用的结果.对行星尺度纬圈平均扰动分量和天气尺度扰动分量用旋转经验正交函数(REOF)展开,不但可以证实人们已经命名的区域性大气涛动,还新发现了北极地区的两对偶极涛动、欧亚涛动(EAO)和"大西洋—欧亚型"(AEA)波列.这些涛动连接了相邻地区的异常天气和异常气候. Atmospheric teleconnections in the Northern Hemisphere such as Arctic Oscillation (AO), North Atlantic Oscillation (NAO) and Pacific-North American (PNA) teleconnection can be explained by the physical decomposition of geopotential height. The result shows that the AO reflects planetary-scale zonal-mean anomalies in the Arctic region; the PNA results from persistent regional-scale atmospheric anomalies; NAO is a combined result of both planetary-scale zonal-mean and regional-scale anomalies. The rotated empirical orthogonal function (REOF) of planetary-scale zonal-mean and regional-scale anomalies not only confirms the already known regional oscillations and wave trains, but also discovers new patterns, such as "twin dipole oscillations" in the Arctic region, Euro-Asia Oscillation (EAO) and Atlantic-Euro-Asia (AEA) wave-train pattern. These oscillations or wave trains are linked to adjacent regional weather anomalies and climate anomalies. SCI(E) 中文核心期刊要目总览(PKU) 中国科技核心期刊(ISTIC) 中国科学引文数据库(CSCD) 0 05 1449-1461 55
author2 北京大学大气海洋科学系
format Journal/Newspaper
author 钱维宏
梁浩原
author_facet 钱维宏
梁浩原
author_sort 钱维宏
title 北半球大气遥相关型与区域尺度大气扰动
title_short 北半球大气遥相关型与区域尺度大气扰动
title_full 北半球大气遥相关型与区域尺度大气扰动
title_fullStr 北半球大气遥相关型与区域尺度大气扰动
title_full_unstemmed 北半球大气遥相关型与区域尺度大气扰动
title_sort 北半球大气遥相关型与区域尺度大气扰动
publisher 地球物理学报
publishDate 2012
url https://hdl.handle.net/20.500.11897/177588
https://doi.org/10.6038/j.issn.0001-5733.2012.05.003
geographic Arctic
Pacific
geographic_facet Arctic
Pacific
genre Arctic
North Atlantic
North Atlantic oscillation
genre_facet Arctic
North Atlantic
North Atlantic oscillation
op_source 万方
知网
SCI
op_relation 地球物理学报.2012,(05),1449-1461.
878498
0001-5733
http://hdl.handle.net/20.500.11897/177588
doi:10.6038/j.issn.0001-5733.2012.05.003
WOS:000304734300003
op_doi https://doi.org/20.500.11897/177588
https://doi.org/10.6038/j.issn.0001-5733.2012.05.003
_version_ 1766330337022967808