The Upstream ＂Strong Signals＂ of the Water Vapor Transport over the Tibetan Plateau during a Heavy Rainfall Event in the Yangtze River Basin
A heavy rainfall event that occurred over the middle and lower reaches of the Yangtze River Basin （YRB） during July 11-13 2000 is explored in this study. The potential/stream function is used to analyze the upstream ＂strong signals＂ of the water vapor transport in the Tibetan Plateau （TP）. The studi...
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| Veröffentlicht in: | Advances in atmospheric sciences 2016-12, Vol.33 (12), p.1343-1350 |
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| description | A heavy rainfall event that occurred over the middle and lower reaches of the Yangtze River Basin （YRB） during July 11-13 2000 is explored in this study. The potential/stream function is used to analyze the upstream ＂strong signals＂ of the water vapor transport in the Tibetan Plateau （TP）. The studied time period covers from 2000 LST 5 July to 2000 LST 15 July （temporal resolution： 6 hours）. By analyzing the three-dimensional structure of the water vapor flux, vorticity and divergence prior to and during the heavy rainfall event, the upstream ＂strong signals＂ related to this heavy rainfall event are revealed. A strong correlation exists between the heavy rainfall event in the YRB and the convective clouds over the TE The ＂convergence zone＂ of the water vapor transport is also identified, based on correlation analysis of the water vapor flux two days and one day prior to, and on the day of, the heavy rainfall. And this ＂convergence zone＂ coincides with the migration of the maximum rainfall over the YRB. This specific coupled structure actually plays a key role in generating heavy rainfall over the YRB. The eastward movement of the coupled system with a divergence]convergence center of the potential function at the upper/lower level resembles the spatiotemporal evolution of the heavy rainfall event over the YRB. These upstream ＂strong signals＂ are clearly traced in this study through analyzing the three-dimensional structure of the potential/stream function of upstream water vapor transport. |
| doi_str_mv | 10.1007/s00376-016-6118-7 |
| format | Article |
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The potential/stream function is used to analyze the upstream ＂strong signals＂ of the water vapor transport in the Tibetan Plateau （TP）. The studied time period covers from 2000 LST 5 July to 2000 LST 15 July （temporal resolution： 6 hours）. By analyzing the three-dimensional structure of the water vapor flux, vorticity and divergence prior to and during the heavy rainfall event, the upstream ＂strong signals＂ related to this heavy rainfall event are revealed. A strong correlation exists between the heavy rainfall event in the YRB and the convective clouds over the TE The ＂convergence zone＂ of the water vapor transport is also identified, based on correlation analysis of the water vapor flux two days and one day prior to, and on the day of, the heavy rainfall. And this ＂convergence zone＂ coincides with the migration of the maximum rainfall over the YRB. This specific coupled structure actually plays a key role in generating heavy rainfall over the YRB. The eastward movement of the coupled system with a divergence]convergence center of the potential function at the upper/lower level resembles the spatiotemporal evolution of the heavy rainfall event over the YRB. These upstream ＂strong signals＂ are clearly traced in this study through analyzing the three-dimensional structure of the potential/stream function of upstream water vapor transport.</description><identifier>ISSN: 0256-1530</identifier><identifier>EISSN: 1861-9533</identifier><identifier>DOI: 10.1007/s00376-016-6118-7</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Atmospheric circulation ; Atmospheric Sciences ; Climate and Weather Extremes ; Clouds ; Correlation analysis ; Earth and Environmental Science ; Earth Sciences ; Evapotranspiration ; Freshwater ; Geophysics/Geodesy ; Meteorology ; Rain ; Rainfall ; River basins ; Rivers ; Upstream ; Water vapor ; 上游 ; 强信号 ; 时间分辨率 ; 暴雨过程 ; 水汽输送 ; 西藏高原 ; 长江流域 ; 降水事件</subject><ispartof>Advances in atmospheric sciences, 2016-12, Vol.33 (12), p.1343-1350</ispartof><rights>Science Press 2016</rights><rights>Chinese National Committee for International Association of Meteorology and Atmospheric Sciences, Institute of Atmospheric Physics, Science Press and Springer-Verlag Berlin Heidelberg 2016</rights><rights>Copyright © Wanfang Data Co. 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All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c410t-38860b2193e8cbeb68dfbbddfd06a4c8a023b610f09f1f2a4a34ed73a2908b363</citedby><cites>FETCH-LOGICAL-c410t-38860b2193e8cbeb68dfbbddfd06a4c8a023b610f09f1f2a4a34ed73a2908b363</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/84334X/84334X.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00376-016-6118-7$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00376-016-6118-7$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids></links><search><creatorcontrib>Zhao, Yang</creatorcontrib><creatorcontrib>Xu, Xiangde</creatorcontrib><creatorcontrib>Chen, Bin</creatorcontrib><creatorcontrib>Wang, Yinjun</creatorcontrib><title>The Upstream ＂Strong Signals＂ of the Water Vapor Transport over the Tibetan Plateau during a Heavy Rainfall Event in the Yangtze River Basin</title><title>Advances in atmospheric sciences</title><addtitle>Adv. Atmos. Sci</addtitle><addtitle>Advances in Atmospheric Sciences</addtitle><description>A heavy rainfall event that occurred over the middle and lower reaches of the Yangtze River Basin （YRB） during July 11-13 2000 is explored in this study. The potential/stream function is used to analyze the upstream ＂strong signals＂ of the water vapor transport in the Tibetan Plateau （TP）. The studied time period covers from 2000 LST 5 July to 2000 LST 15 July （temporal resolution： 6 hours）. By analyzing the three-dimensional structure of the water vapor flux, vorticity and divergence prior to and during the heavy rainfall event, the upstream ＂strong signals＂ related to this heavy rainfall event are revealed. A strong correlation exists between the heavy rainfall event in the YRB and the convective clouds over the TE The ＂convergence zone＂ of the water vapor transport is also identified, based on correlation analysis of the water vapor flux two days and one day prior to, and on the day of, the heavy rainfall. And this ＂convergence zone＂ coincides with the migration of the maximum rainfall over the YRB. This specific coupled structure actually plays a key role in generating heavy rainfall over the YRB. The eastward movement of the coupled system with a divergence]convergence center of the potential function at the upper/lower level resembles the spatiotemporal evolution of the heavy rainfall event over the YRB. These upstream ＂strong signals＂ are clearly traced in this study through analyzing the three-dimensional structure of the potential/stream function of upstream water vapor transport.</description><subject>Atmospheric circulation</subject><subject>Atmospheric Sciences</subject><subject>Climate and Weather Extremes</subject><subject>Clouds</subject><subject>Correlation analysis</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Evapotranspiration</subject><subject>Freshwater</subject><subject>Geophysics/Geodesy</subject><subject>Meteorology</subject><subject>Rain</subject><subject>Rainfall</subject><subject>River basins</subject><subject>Rivers</subject><subject>Upstream</subject><subject>Water vapor</subject><subject>上游</subject><subject>强信号</subject><subject>时间分辨率</subject><subject>暴雨过程</subject><subject>水汽输送</subject><subject>西藏高原</subject><subject>长江流域</subject><subject>降水事件</subject><issn>0256-1530</issn><issn>1861-9533</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9ksFu1DAQhiMEEkvhAbhZcIFDYMZOHOcIVaFIlUDtFsTJmmycbZask7Wdpe2xT8AD8U68Ag6pKsSBky37-_8Zz-8keYrwCgGK1x5AFDIFlKlEVGlxL1mgkpiWuRD3kwXwXKaYC3iYPPJ-E-lSKFwkP5YXhp0PPjhDW_br581ZcL1ds7N2banz8YD1DQsR-kLBOPaZht6xpSPr4yawfh8Pp-tlW5lAln3qIkcjq0fXRh9ix4b2V-yUWttQ17GjvbGBtfaP6CvZdbg27LSdbN6Sb-3j5EHkvHlyux4k5--OlofH6cnH9x8O35ykqwwhpEIpCRXHUhi1qkwlVd1UVV03NUjKVoqAi0oiNFA22HDKSGSmLgTxElQlpDhIXs6-3yk2Ztd6049uerKud98uN9fa8DhM5ABZZF_M7OD63Wh80NvWr0zXkTX96DWqTGaYlQIi-vwf9M4XlVBlkfGcRwpnauV6751p9ODaLbkrjaCnPPWcp44t6ClPXUQNnzV-mCZr3F_O_xE9uy10EVPdRd1dJVmAzDGP3-M3q8mwqA</recordid><startdate>20161201</startdate><enddate>20161201</enddate><creator>Zhao, Yang</creator><creator>Xu, Xiangde</creator><creator>Chen, Bin</creator><creator>Wang, Yinjun</creator><general>Science Press</general><general>Springer Nature B.V</general><general>Nanjing University of Information Science & Technology, Jiangsu 210044, China</general><general>State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, China%State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, China</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7XB</scope><scope>88F</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M1Q</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>7UA</scope><scope>C1K</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20161201</creationdate><title>The Upstream ＂Strong Signals＂ of the Water Vapor Transport over the Tibetan Plateau during a Heavy Rainfall Event in the Yangtze River Basin</title><author>Zhao, Yang ; Xu, Xiangde ; Chen, Bin ; Wang, Yinjun</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c410t-38860b2193e8cbeb68dfbbddfd06a4c8a023b610f09f1f2a4a34ed73a2908b363</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Atmospheric circulation</topic><topic>Atmospheric Sciences</topic><topic>Climate and Weather Extremes</topic><topic>Clouds</topic><topic>Correlation analysis</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Evapotranspiration</topic><topic>Freshwater</topic><topic>Geophysics/Geodesy</topic><topic>Meteorology</topic><topic>Rain</topic><topic>Rainfall</topic><topic>River basins</topic><topic>Rivers</topic><topic>Upstream</topic><topic>Water vapor</topic><topic>上游</topic><topic>强信号</topic><topic>时间分辨率</topic><topic>暴雨过程</topic><topic>水汽输送</topic><topic>西藏高原</topic><topic>长江流域</topic><topic>降水事件</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhao, Yang</creatorcontrib><creatorcontrib>Xu, Xiangde</creatorcontrib><creatorcontrib>Chen, Bin</creatorcontrib><creatorcontrib>Wang, Yinjun</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Military Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Military Database</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Advances in atmospheric sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhao, Yang</au><au>Xu, Xiangde</au><au>Chen, Bin</au><au>Wang, Yinjun</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Upstream ＂Strong Signals＂ of the Water Vapor Transport over the Tibetan Plateau during a Heavy Rainfall Event in the Yangtze River Basin</atitle><jtitle>Advances in atmospheric sciences</jtitle><stitle>Adv. Atmos. Sci</stitle><addtitle>Advances in Atmospheric Sciences</addtitle><date>2016-12-01</date><risdate>2016</risdate><volume>33</volume><issue>12</issue><spage>1343</spage><epage>1350</epage><pages>1343-1350</pages><issn>0256-1530</issn><eissn>1861-9533</eissn><abstract>A heavy rainfall event that occurred over the middle and lower reaches of the Yangtze River Basin （YRB） during July 11-13 2000 is explored in this study. The potential/stream function is used to analyze the upstream ＂strong signals＂ of the water vapor transport in the Tibetan Plateau （TP）. The studied time period covers from 2000 LST 5 July to 2000 LST 15 July （temporal resolution： 6 hours）. By analyzing the three-dimensional structure of the water vapor flux, vorticity and divergence prior to and during the heavy rainfall event, the upstream ＂strong signals＂ related to this heavy rainfall event are revealed. A strong correlation exists between the heavy rainfall event in the YRB and the convective clouds over the TE The ＂convergence zone＂ of the water vapor transport is also identified, based on correlation analysis of the water vapor flux two days and one day prior to, and on the day of, the heavy rainfall. And this ＂convergence zone＂ coincides with the migration of the maximum rainfall over the YRB. This specific coupled structure actually plays a key role in generating heavy rainfall over the YRB. The eastward movement of the coupled system with a divergence]convergence center of the potential function at the upper/lower level resembles the spatiotemporal evolution of the heavy rainfall event over the YRB. These upstream ＂strong signals＂ are clearly traced in this study through analyzing the three-dimensional structure of the potential/stream function of upstream water vapor transport.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s00376-016-6118-7</doi><tpages>8</tpages></addata></record> |
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| ispartof | Advances in atmospheric sciences, 2016-12, Vol.33 (12), p.1343-1350 |
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| subjects | Atmospheric circulation Atmospheric Sciences Climate and Weather Extremes Clouds Correlation analysis Earth and Environmental Science Earth Sciences Evapotranspiration Freshwater Geophysics/Geodesy Meteorology Rain Rainfall River basins Rivers Upstream Water vapor 上游 强信号 时间分辨率 暴雨过程 水汽输送 西藏高原 长江流域 降水事件 |
| title | The Upstream ＂Strong Signals＂ of the Water Vapor Transport over the Tibetan Plateau during a Heavy Rainfall Event in the Yangtze River Basin |
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