Decreasing Influence of Summer Snow Cover Over the Western Tibetan Plateau on East Asian Precipitation Under Global Warming

In recent years, some studies emphasized the influence of western Tibetan Plateau summer snow on the East Asian summer precipitation. With the temperature rise in the past decades, the snow cover over the western Tibetan Plateau in summer has significantly decreased. This raises the question whether...

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Autores principales: Zhibiao Wang, Renguang Wu, Zhang Chen, Lihua Zhu, Kai Yang, Kui Liu, Yiya Yang
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Lenguaje:EN
Publicado: Frontiers Media S.A. 2021
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spelling oai:doaj.org-article:0b465200af7c4134b3c35bec6d9c1f832021-12-01T02:31:48ZDecreasing Influence of Summer Snow Cover Over the Western Tibetan Plateau on East Asian Precipitation Under Global Warming2296-646310.3389/feart.2021.787971https://doaj.org/article/0b465200af7c4134b3c35bec6d9c1f832021-11-01T00:00:00Zhttps://www.frontiersin.org/articles/10.3389/feart.2021.787971/fullhttps://doaj.org/toc/2296-6463In recent years, some studies emphasized the influence of western Tibetan Plateau summer snow on the East Asian summer precipitation. With the temperature rise in the past decades, the snow cover over the western Tibetan Plateau in summer has significantly decreased. This raises the question whether the impact of the Tibetan Plateau snow has changed. The present study identifies a prominent change in the influence of the western Tibetan Plateau snow cover on the East Asian summer precipitation. Before the early 2000’s, positive precipitation anomalies extend from the southeastern Tibetan Plateau through the Yangtze River to Japan and Korea and negative anomalies cover southeast China corresponding to more Tibetan Plateau snow cover. After the early 2000’s, with the reduction of snow cover variability, below-normal and above-normal summer precipitation occurs over northern China-Mongolia and northeast Asia, respectively, corresponding to more Tibetan Plateau snow cover. The change in the influence of the Tibetan Plateau snow on the East Asian summer precipitation is associated with an obvious change in the atmospheric circulation anomaly pattern. Before the early 2000’s, the wind anomalies display a south-north contrast pattern with anomalous convergence along the Yangtze River. After the early 2000’s, an anomalous cyclone occupies Northeast China with anomalous southerlies and northerlies over northeast Asia and northern China, respectively. The Tibetan Plateau snow cover variation after the early 2000’s is associated with the northeast Indian summer precipitation. The model experiments confirm that the weakened influence of summer western Tibetan Plateau snow cover on the East Asian atmospheric circulation and precipitation with the reduced snow cover anomalies.Zhibiao WangRenguang WuRenguang WuZhang ChenLihua ZhuKai YangKui LiuYiya YangFrontiers Media S.A.articletibetan plateau summer snow covereast asian summer precipitationglobal warmingnortheast indian precipitationweakened influenceScienceQENFrontiers in Earth Science, Vol 9 (2021)
institution DOAJ
collection DOAJ
language EN
topic tibetan plateau summer snow cover
east asian summer precipitation
global warming
northeast indian precipitation
weakened influence
Science
Q
spellingShingle tibetan plateau summer snow cover
east asian summer precipitation
global warming
northeast indian precipitation
weakened influence
Science
Q
Zhibiao Wang
Renguang Wu
Renguang Wu
Zhang Chen
Lihua Zhu
Kai Yang
Kui Liu
Yiya Yang
Decreasing Influence of Summer Snow Cover Over the Western Tibetan Plateau on East Asian Precipitation Under Global Warming
description In recent years, some studies emphasized the influence of western Tibetan Plateau summer snow on the East Asian summer precipitation. With the temperature rise in the past decades, the snow cover over the western Tibetan Plateau in summer has significantly decreased. This raises the question whether the impact of the Tibetan Plateau snow has changed. The present study identifies a prominent change in the influence of the western Tibetan Plateau snow cover on the East Asian summer precipitation. Before the early 2000’s, positive precipitation anomalies extend from the southeastern Tibetan Plateau through the Yangtze River to Japan and Korea and negative anomalies cover southeast China corresponding to more Tibetan Plateau snow cover. After the early 2000’s, with the reduction of snow cover variability, below-normal and above-normal summer precipitation occurs over northern China-Mongolia and northeast Asia, respectively, corresponding to more Tibetan Plateau snow cover. The change in the influence of the Tibetan Plateau snow on the East Asian summer precipitation is associated with an obvious change in the atmospheric circulation anomaly pattern. Before the early 2000’s, the wind anomalies display a south-north contrast pattern with anomalous convergence along the Yangtze River. After the early 2000’s, an anomalous cyclone occupies Northeast China with anomalous southerlies and northerlies over northeast Asia and northern China, respectively. The Tibetan Plateau snow cover variation after the early 2000’s is associated with the northeast Indian summer precipitation. The model experiments confirm that the weakened influence of summer western Tibetan Plateau snow cover on the East Asian atmospheric circulation and precipitation with the reduced snow cover anomalies.
format article
author Zhibiao Wang
Renguang Wu
Renguang Wu
Zhang Chen
Lihua Zhu
Kai Yang
Kui Liu
Yiya Yang
author_facet Zhibiao Wang
Renguang Wu
Renguang Wu
Zhang Chen
Lihua Zhu
Kai Yang
Kui Liu
Yiya Yang
author_sort Zhibiao Wang
title Decreasing Influence of Summer Snow Cover Over the Western Tibetan Plateau on East Asian Precipitation Under Global Warming
title_short Decreasing Influence of Summer Snow Cover Over the Western Tibetan Plateau on East Asian Precipitation Under Global Warming
title_full Decreasing Influence of Summer Snow Cover Over the Western Tibetan Plateau on East Asian Precipitation Under Global Warming
title_fullStr Decreasing Influence of Summer Snow Cover Over the Western Tibetan Plateau on East Asian Precipitation Under Global Warming
title_full_unstemmed Decreasing Influence of Summer Snow Cover Over the Western Tibetan Plateau on East Asian Precipitation Under Global Warming
title_sort decreasing influence of summer snow cover over the western tibetan plateau on east asian precipitation under global warming
publisher Frontiers Media S.A.
publishDate 2021
url https://doaj.org/article/0b465200af7c4134b3c35bec6d9c1f83
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