Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century

[1] At odds with global warming trends, surface air temperature over large subtropical Eurasia continent in spring March exhibits unique strong cooling over the last half century. The cause for this cooling is shown to be related to Winter (DJF) North Atlantic Oscillation (W-NAO). Positive values of...

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Bibliographic Details
Main Authors: Rucong Yu, Tianjun Zhou
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2004
Subjects:
North Atlantic
North Atlantic oscillation
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.462.5317
http://www.lasg.ac.cn/UpLoadFiles/File/papers/2004/2004grl_yrc_nao.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.462.5317 2023-05-15T17:30:32+02:00 Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century Rucong Yu Tianjun Zhou The Pennsylvania State University CiteSeerX Archives 2004 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.462.5317 http://www.lasg.ac.cn/UpLoadFiles/File/papers/2004/2004grl_yrc_nao.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.462.5317 http://www.lasg.ac.cn/UpLoadFiles/File/papers/2004/2004grl_yrc_nao.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.lasg.ac.cn/UpLoadFiles/File/papers/2004/2004grl_yrc_nao.pdf text 2004 ftciteseerx 2016-10-16T00:04:47Z [1] At odds with global warming trends, surface air temperature over large subtropical Eurasia continent in spring March exhibits unique strong cooling over the last half century. The cause for this cooling is shown to be related to Winter (DJF) North Atlantic Oscillation (W-NAO). Positive values of W-NAO provoke cooling signals in northern Africa continent simultaneously from surface to tropopause. The W-NAO generated signals barotropically extend eastward over most of subtropical Eurasia and Text North Atlantic North Atlantic oscillation Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description [1] At odds with global warming trends, surface air temperature over large subtropical Eurasia continent in spring March exhibits unique strong cooling over the last half century. The cause for this cooling is shown to be related to Winter (DJF) North Atlantic Oscillation (W-NAO). Positive values of W-NAO provoke cooling signals in northern Africa continent simultaneously from surface to tropopause. The W-NAO generated signals barotropically extend eastward over most of subtropical Eurasia and
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Rucong Yu
Tianjun Zhou
spellingShingle Rucong Yu
Tianjun Zhou
Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century
author_facet Rucong Yu
Tianjun Zhou
author_sort Rucong Yu
title Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century
title_short Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century
title_full Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century
title_fullStr Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century
title_full_unstemmed Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century
title_sort impacts of winter-nao on march cooling trends over subtropical eurasia continent in the recent half century
publishDate 2004
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.462.5317
http://www.lasg.ac.cn/UpLoadFiles/File/papers/2004/2004grl_yrc_nao.pdf
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source http://www.lasg.ac.cn/UpLoadFiles/File/papers/2004/2004grl_yrc_nao.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.462.5317
http://www.lasg.ac.cn/UpLoadFiles/File/papers/2004/2004grl_yrc_nao.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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