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A vertical transport window of water vapor in the troposphere over the Tibetan Plateau with implications for global climate change
By using the multi-source data of meteorology over recent decades, this study discovered a summertime “hollow wet pool” in the troposphere with a center of high water vapor over the Asian water tower (AWT) on the Tibetan Plateau (TP), which is indicated by a vertical transport “window” in the tropos...
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Published in: | Atmospheric chemistry and physics 2022-01, Vol.22 (2), p.1149-1157 |
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container_end_page | 1157 |
container_issue | 2 |
container_start_page | 1149 |
container_title | Atmospheric chemistry and physics |
container_volume | 22 |
creator | Xu, Xiangde Sun, Chan Chen, Deliang Zhao, Tianliang Xu, Jianjun Zhang, Shengjun Li, Juan Chen, Bin Zhao, Yang Xu, Hongxiong Dong, Lili Sun, Xiaoyun Zhu, Yan |
description | By using the multi-source data of meteorology over recent decades, this
study discovered a summertime “hollow wet pool” in the troposphere with a
center of high water vapor over the Asian water tower (AWT) on the Tibetan
Plateau (TP), which is indicated by a vertical transport “window” in the
troposphere. The water vapor transport in the upper troposphere extends from
the vertical transport window over the TP with significant connections
among the Arctic, Antarctic and TP regions, highlighting the effect of the TP's
vertical transport window of water vapor in the troposphere on global change
in water vapor. The vertical transport window is built by the AWT's thermal
forcing in association with the dynamic effect of the TP's “hollow heat
island”. Our study improves the understanding of the vapor transport over
the TP with important implication for global climate change. |
doi_str_mv | 10.5194/acp-22-1149-2022 |
format | article |
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study discovered a summertime “hollow wet pool” in the troposphere with a
center of high water vapor over the Asian water tower (AWT) on the Tibetan
Plateau (TP), which is indicated by a vertical transport “window” in the
troposphere. The water vapor transport in the upper troposphere extends from
the vertical transport window over the TP with significant connections
among the Arctic, Antarctic and TP regions, highlighting the effect of the TP's
vertical transport window of water vapor in the troposphere on global change
in water vapor. The vertical transport window is built by the AWT's thermal
forcing in association with the dynamic effect of the TP's “hollow heat
island”. Our study improves the understanding of the vapor transport over
the TP with important implication for global climate change.</description><identifier>ISSN: 1680-7324</identifier><identifier>ISSN: 1680-7316</identifier><identifier>EISSN: 1680-7324</identifier><identifier>DOI: 10.5194/acp-22-1149-2022</identifier><language>eng</language><publisher>Katlenburg-Lindau: Copernicus GmbH</publisher><subject>Climate change ; Clouds ; Earth and Related Environmental Sciences ; Environmental aspects ; Geovetenskap och miljövetenskap ; Global climate ; Global temperature changes ; Heat ; Heat islands ; Meteorology ; Polar environments ; Precipitation ; Remote sensing ; Rivers ; Stratosphere ; Troposphere ; Tropospheric water vapor ; Upper troposphere ; Urban heat islands ; Vertical advection ; Water towers ; Water vapor ; Water vapor transport ; Water vapour</subject><ispartof>Atmospheric chemistry and physics, 2022-01, Vol.22 (2), p.1149-1157</ispartof><rights>COPYRIGHT 2022 Copernicus GmbH</rights><rights>2022. This work is published under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c518t-a88c9aeb710033383da8670847b11c3c5c5a92470dbd44fad225e8560647d8263</citedby><cites>FETCH-LOGICAL-c518t-a88c9aeb710033383da8670847b11c3c5c5a92470dbd44fad225e8560647d8263</cites><orcidid>0000-0002-8608-4131 ; 0000-0003-0288-5618</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2622194278/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2622194278?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>230,314,780,784,864,885,2102,25753,27924,27925,37012,44590,75126</link.rule.ids><backlink>$$Uhttps://gup.ub.gu.se/publication/314244$$DView record from Swedish Publication Index$$Hfree_for_read</backlink></links><search><creatorcontrib>Xu, Xiangde</creatorcontrib><creatorcontrib>Sun, Chan</creatorcontrib><creatorcontrib>Chen, Deliang</creatorcontrib><creatorcontrib>Zhao, Tianliang</creatorcontrib><creatorcontrib>Xu, Jianjun</creatorcontrib><creatorcontrib>Zhang, Shengjun</creatorcontrib><creatorcontrib>Li, Juan</creatorcontrib><creatorcontrib>Chen, Bin</creatorcontrib><creatorcontrib>Zhao, Yang</creatorcontrib><creatorcontrib>Xu, Hongxiong</creatorcontrib><creatorcontrib>Dong, Lili</creatorcontrib><creatorcontrib>Sun, Xiaoyun</creatorcontrib><creatorcontrib>Zhu, Yan</creatorcontrib><title>A vertical transport window of water vapor in the troposphere over the Tibetan Plateau with implications for global climate change</title><title>Atmospheric chemistry and physics</title><description>By using the multi-source data of meteorology over recent decades, this
study discovered a summertime “hollow wet pool” in the troposphere with a
center of high water vapor over the Asian water tower (AWT) on the Tibetan
Plateau (TP), which is indicated by a vertical transport “window” in the
troposphere. The water vapor transport in the upper troposphere extends from
the vertical transport window over the TP with significant connections
among the Arctic, Antarctic and TP regions, highlighting the effect of the TP's
vertical transport window of water vapor in the troposphere on global change
in water vapor. The vertical transport window is built by the AWT's thermal
forcing in association with the dynamic effect of the TP's “hollow heat
island”. Our study improves the understanding of the vapor transport over
the TP with important implication for global climate change.</description><subject>Climate change</subject><subject>Clouds</subject><subject>Earth and Related Environmental Sciences</subject><subject>Environmental aspects</subject><subject>Geovetenskap och miljövetenskap</subject><subject>Global climate</subject><subject>Global temperature changes</subject><subject>Heat</subject><subject>Heat islands</subject><subject>Meteorology</subject><subject>Polar environments</subject><subject>Precipitation</subject><subject>Remote sensing</subject><subject>Rivers</subject><subject>Stratosphere</subject><subject>Troposphere</subject><subject>Tropospheric water vapor</subject><subject>Upper troposphere</subject><subject>Urban heat islands</subject><subject>Vertical advection</subject><subject>Water towers</subject><subject>Water vapor</subject><subject>Water vapor transport</subject><subject>Water 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Juan</au><au>Chen, Bin</au><au>Zhao, Yang</au><au>Xu, Hongxiong</au><au>Dong, Lili</au><au>Sun, Xiaoyun</au><au>Zhu, Yan</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A vertical transport window of water vapor in the troposphere over the Tibetan Plateau with implications for global climate change</atitle><jtitle>Atmospheric chemistry and physics</jtitle><date>2022-01-24</date><risdate>2022</risdate><volume>22</volume><issue>2</issue><spage>1149</spage><epage>1157</epage><pages>1149-1157</pages><issn>1680-7324</issn><issn>1680-7316</issn><eissn>1680-7324</eissn><abstract>By using the multi-source data of meteorology over recent decades, this
study discovered a summertime “hollow wet pool” in the troposphere with a
center of high water vapor over the Asian water tower (AWT) on the Tibetan
Plateau (TP), which is indicated by a vertical transport “window” in the
troposphere. The water vapor transport in the upper troposphere extends from
the vertical transport window over the TP with significant connections
among the Arctic, Antarctic and TP regions, highlighting the effect of the TP's
vertical transport window of water vapor in the troposphere on global change
in water vapor. The vertical transport window is built by the AWT's thermal
forcing in association with the dynamic effect of the TP's “hollow heat
island”. Our study improves the understanding of the vapor transport over
the TP with important implication for global climate change.</abstract><cop>Katlenburg-Lindau</cop><pub>Copernicus GmbH</pub><doi>10.5194/acp-22-1149-2022</doi><tpages>9</tpages><orcidid>https://orcid.org/0000-0002-8608-4131</orcidid><orcidid>https://orcid.org/0000-0003-0288-5618</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Climate change Clouds Earth and Related Environmental Sciences Environmental aspects Geovetenskap och miljövetenskap Global climate Global temperature changes Heat Heat islands Meteorology Polar environments Precipitation Remote sensing Rivers Stratosphere Troposphere Tropospheric water vapor Upper troposphere Urban heat islands Vertical advection Water towers Water vapor Water vapor transport Water vapour |
title | A vertical transport window of water vapor in the troposphere over the Tibetan Plateau with implications for global climate change |
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