On The Contribution of Arctic Sea-Ice,ENSO,and Arctic Oscillation over East Asian Cold Winters

The relationships between Arctic Oscillation(AO) and East Asian cold winter have been comprehensively investigated during the last decade.More than that,it is suggested that most of the extreme phases of AO can be attributed to the downward propagation of Northern Annular Mode(NAM) from the strat. 中...

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Bibliographic Details
Main Authors: WEN Xinyu, HU Yongyun, LIU Jiping
Other Authors: Dept of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Dept of Atmospheric and Environmental Sciences, University at Albany, State University of New York, NY, U.S.A., 12222
Format: Conference Object
Language:English
Published: 2013
Subjects:
Arctic
winter
extreme
autumn
ENSO
seasonal
unstable
attributed
polar
forcing
Sea ice
Online Access:https://hdl.handle.net/20.500.11897/444599
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spelling ftpekinguniv:oai:localhost:20.500.11897/444599 2023-05-15T14:32:45+02:00 On The Contribution of Arctic Sea-Ice,ENSO,and Arctic Oscillation over East Asian Cold Winters WEN Xinyu HU Yongyun LIU Jiping Dept of Atmospheric and Oceanic Sciences School of Physics Peking University Dept of Atmospheric and Environmental Sciences University at Albany State University of New York NY U.S.A. 12222 2013 https://hdl.handle.net/20.500.11897/444599 en eng 中国江苏南京. 1409743 http://hdl.handle.net/20.500.11897/444599 知网 Arctic winter extreme autumn ENSO seasonal unstable attributed polar forcing Conference 2013 ftpekinguniv https://doi.org/20.500.11897/444599 2021-08-01T10:54:46Z The relationships between Arctic Oscillation(AO) and East Asian cold winter have been comprehensively investigated during the last decade.More than that,it is suggested that most of the extreme phases of AO can be attributed to the downward propagation of Northern Annular Mode(NAM) from the strat. 中国气象局 1 Conference Object Arctic Sea ice Peking University Institutional Repository (PKU IR) Arctic
institution Open Polar
collection Peking University Institutional Repository (PKU IR)
op_collection_id ftpekinguniv
language English
topic Arctic
winter
extreme
autumn
ENSO
seasonal
unstable
attributed
polar
forcing
spellingShingle Arctic
winter
extreme
autumn
ENSO
seasonal
unstable
attributed
polar
forcing
WEN Xinyu
HU Yongyun
LIU Jiping
On The Contribution of Arctic Sea-Ice,ENSO,and Arctic Oscillation over East Asian Cold Winters
topic_facet Arctic
winter
extreme
autumn
ENSO
seasonal
unstable
attributed
polar
forcing
description The relationships between Arctic Oscillation(AO) and East Asian cold winter have been comprehensively investigated during the last decade.More than that,it is suggested that most of the extreme phases of AO can be attributed to the downward propagation of Northern Annular Mode(NAM) from the strat. 中国气象局 1
author2 Dept of Atmospheric and Oceanic Sciences
School of Physics
Peking University
Dept of Atmospheric and Environmental Sciences
University at Albany
State University of New York
NY
U.S.A.
12222
format Conference Object
author WEN Xinyu
HU Yongyun
LIU Jiping
author_facet WEN Xinyu
HU Yongyun
LIU Jiping
author_sort WEN Xinyu
title On The Contribution of Arctic Sea-Ice,ENSO,and Arctic Oscillation over East Asian Cold Winters
title_short On The Contribution of Arctic Sea-Ice,ENSO,and Arctic Oscillation over East Asian Cold Winters
title_full On The Contribution of Arctic Sea-Ice,ENSO,and Arctic Oscillation over East Asian Cold Winters
title_fullStr On The Contribution of Arctic Sea-Ice,ENSO,and Arctic Oscillation over East Asian Cold Winters
title_full_unstemmed On The Contribution of Arctic Sea-Ice,ENSO,and Arctic Oscillation over East Asian Cold Winters
title_sort on the contribution of arctic sea-ice,enso,and arctic oscillation over east asian cold winters
publishDate 2013
url https://hdl.handle.net/20.500.11897/444599
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_source 知网
op_relation 中国江苏南京.
1409743
http://hdl.handle.net/20.500.11897/444599
op_doi https://doi.org/20.500.11897/444599
_version_ 1766306111778979840

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