Impact of Autumn-Winter Tibetan Plateau Snow Cover Anomalies on the East Asian Winter Monsoon and Its Interdecadal Change
The present study investigates the impacts of autumn-winter Tibetan Plateau (TP) snow cover anomalies on the interannual variability of the East Asian winter monsoon (EAWM). It is found that the northern component of EAWM is significantly associated with October-November-December-January (ONDJ) snow...
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ftdoajarticles:oai:doaj.org/article:777664eaef1c41e4af282fc2bceb7b05 2023-05-15T13:14:53+02:00 Impact of Autumn-Winter Tibetan Plateau Snow Cover Anomalies on the East Asian Winter Monsoon and Its Interdecadal Change Zhang Chen Renguang Wu Zhibiao Wang 2021-07-01T00:00:00Z https://doi.org/10.3389/feart.2021.699358 https://doaj.org/article/777664eaef1c41e4af282fc2bceb7b05 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/feart.2021.699358/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2021.699358 https://doaj.org/article/777664eaef1c41e4af282fc2bceb7b05 Frontiers in Earth Science, Vol 9 (2021) East asian winter monsoon tibetan plateau snow cover persistence of snow cover anomalies interdecadal change aleutian low Science Q article 2021 ftdoajarticles https://doi.org/10.3389/feart.2021.699358 2022-12-31T05:41:43Z The present study investigates the impacts of autumn-winter Tibetan Plateau (TP) snow cover anomalies on the interannual variability of the East Asian winter monsoon (EAWM). It is found that the northern component of EAWM is significantly associated with October-November-December-January (ONDJ) snow cover anomalies over the eastern TP, whereas the TP snow cover changes have little impact on the southern component of EAWM. However, the relationship of the northern component of EAWM to ONDJ TP snow cover experienced an obvious change in the mid-1990s. During 1979–1998, due to the high persistence of TP snow anomalies from autumn to winter, extensive ONDJ TP snow cover anomalies have a prominent influence on atmospheric circulation over Asia and the North Pacific, with more TP snow cover followed by an enhanced Siberian high and a deepened Aleutian low in winter, resulting in stronger EAWM. During 1999–2016, TP snow cover anomalies have a weak persistence. The atmospheric circulation anomalies display a different distribution. As such, there is a weak connection between the northern component of EAWM and the TP snow cover anomalies during this period. Article in Journal/Newspaper aleutian low Directory of Open Access Journals: DOAJ Articles Pacific Frontiers in Earth Science 9 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
East asian winter monsoon tibetan plateau snow cover persistence of snow cover anomalies interdecadal change aleutian low Science Q |
spellingShingle |
East asian winter monsoon tibetan plateau snow cover persistence of snow cover anomalies interdecadal change aleutian low Science Q Zhang Chen Renguang Wu Zhibiao Wang Impact of Autumn-Winter Tibetan Plateau Snow Cover Anomalies on the East Asian Winter Monsoon and Its Interdecadal Change |
topic_facet |
East asian winter monsoon tibetan plateau snow cover persistence of snow cover anomalies interdecadal change aleutian low Science Q |
description |
The present study investigates the impacts of autumn-winter Tibetan Plateau (TP) snow cover anomalies on the interannual variability of the East Asian winter monsoon (EAWM). It is found that the northern component of EAWM is significantly associated with October-November-December-January (ONDJ) snow cover anomalies over the eastern TP, whereas the TP snow cover changes have little impact on the southern component of EAWM. However, the relationship of the northern component of EAWM to ONDJ TP snow cover experienced an obvious change in the mid-1990s. During 1979–1998, due to the high persistence of TP snow anomalies from autumn to winter, extensive ONDJ TP snow cover anomalies have a prominent influence on atmospheric circulation over Asia and the North Pacific, with more TP snow cover followed by an enhanced Siberian high and a deepened Aleutian low in winter, resulting in stronger EAWM. During 1999–2016, TP snow cover anomalies have a weak persistence. The atmospheric circulation anomalies display a different distribution. As such, there is a weak connection between the northern component of EAWM and the TP snow cover anomalies during this period. |
format |
Article in Journal/Newspaper |
author |
Zhang Chen Renguang Wu Zhibiao Wang |
author_facet |
Zhang Chen Renguang Wu Zhibiao Wang |
author_sort |
Zhang Chen |
title |
Impact of Autumn-Winter Tibetan Plateau Snow Cover Anomalies on the East Asian Winter Monsoon and Its Interdecadal Change |
title_short |
Impact of Autumn-Winter Tibetan Plateau Snow Cover Anomalies on the East Asian Winter Monsoon and Its Interdecadal Change |
title_full |
Impact of Autumn-Winter Tibetan Plateau Snow Cover Anomalies on the East Asian Winter Monsoon and Its Interdecadal Change |
title_fullStr |
Impact of Autumn-Winter Tibetan Plateau Snow Cover Anomalies on the East Asian Winter Monsoon and Its Interdecadal Change |
title_full_unstemmed |
Impact of Autumn-Winter Tibetan Plateau Snow Cover Anomalies on the East Asian Winter Monsoon and Its Interdecadal Change |
title_sort |
impact of autumn-winter tibetan plateau snow cover anomalies on the east asian winter monsoon and its interdecadal change |
publisher |
Frontiers Media S.A. |
publishDate |
2021 |
url |
https://doi.org/10.3389/feart.2021.699358 https://doaj.org/article/777664eaef1c41e4af282fc2bceb7b05 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
aleutian low |
genre_facet |
aleutian low |
op_source |
Frontiers in Earth Science, Vol 9 (2021) |
op_relation |
https://www.frontiersin.org/articles/10.3389/feart.2021.699358/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2021.699358 https://doaj.org/article/777664eaef1c41e4af282fc2bceb7b05 |
op_doi |
https://doi.org/10.3389/feart.2021.699358 |
container_title |
Frontiers in Earth Science |
container_volume |
9 |
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