Vertical Structures of Atmospheric Properties in Southeast Tibet during the South Asian Summer Monsoon in 2013
In June 2013,a field experiment was conducted in Southeast Tibet in which the air temperature,moisture,and wind were measured by using a GPS sounding system.In the present study,based on these observations and ERA-Interim reanalysis data,the vertical structures of these atmospheric properties and th...
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| Veröffentlicht in: | Acta meteorologica Sinica 2016-04, Vol.30 (2), p.258-264 |
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| creator | 周立波 李斐 朱金焕 邹捍 马舒坡 李鹏 |
| description | In June 2013,a field experiment was conducted in Southeast Tibet in which the air temperature,moisture,and wind were measured by using a GPS sounding system.In the present study,based on these observations and ERA-Interim reanalysis data,the vertical structures of these atmospheric properties and the possible influence of the South Asian summer monsoon（SASM） were investigated.On average,the temperature had a lapse rate of 6.8℃ km~（-1） below the tropopause of 18.0 km.A strong moisture inversion occurred at the near-surface,with a strength of 1.7 g kg~（-1）（100 m）~（-1） for specific humidity.During the observation period,the SASM experienced a south phase and a north phase in the middle and by the end of June,respectively.The monsoon＇s evolution led to large changes in convection and circulation over Southeast Tibet,which further affected the local thermal,moisture,and circulation conditions.The strong convection resulted in an elevated tropopause height over Southeast Tibet during the north phase of the SASM,and the large-scale warm and wet air masses delivered by the monsoon caused high local temperature and moisture conditions. |
| doi_str_mv | 10.1007/s13351-016-5095-1 |
| format | Article |
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Monsoon in 2013</title><title>Acta meteorologica Sinica</title><addtitle>J Meteorol Res</addtitle><addtitle>Acta Meteorologica Sinica</addtitle><description>In June 2013,a field experiment was conducted in Southeast Tibet in which the air temperature,moisture,and wind were measured by using a GPS sounding system.In the present study,based on these observations and ERA-Interim reanalysis data,the vertical structures of these atmospheric properties and the possible influence of the South Asian summer monsoon（SASM） were investigated.On average,the temperature had a lapse rate of 6.8℃ km~（-1） below the tropopause of 18.0 km.A strong moisture inversion occurred at the near-surface,with a strength of 1.7 g kg~（-1）（100 m）~（-1） for specific humidity.During the observation period,the SASM experienced a south phase and a north phase in the middle and by the end of June,respectively.The monsoon＇s evolution led to large changes in convection and circulation over Southeast Tibet,which further affected the local thermal,moisture,and circulation conditions.The strong convection resulted in an elevated tropopause height over Southeast Tibet during the north phase of the SASM,and the large-scale warm and wet air masses delivered by the monsoon caused high local temperature and moisture conditions.</description><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Atmospheric Sciences</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geophysics and Environmental Physics</subject><subject>Meteorology</subject><subject>南亚夏季风</subject><subject>垂直结构</subject><subject>大气参数</subject><subject>季风期</subject><subject>对流层顶</subject><subject>性质</subject><subject>水分条件</subject><subject>西藏东南部</subject><issn>2095-6037</issn><issn>0894-0525</issn><issn>2198-0934</issn><issn>2191-4788</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNp9UU1v1DAQtRBIVNv-AG4WF7gEZmzHTo6rCgpSEUgtXC3HcXZTbeys7ajl3-MoFdw4zWjmfYzmEfIG4QMCqI8JOa-xApRVDW1d4QtywbBtKmi5eFn6dSiBq9fkKqUHAGAtqxVjF8T_cjGP1pzoXY6LzUt0iYaB7vMU0nx0cbT0Rwzziiqb0dO7sOSjMynT-7FzmfZLHP2Bltm2ovs0mgJbpslF-i34FIJfiQyQX5JXgzkld_Vcd-Tn50_311-q2-83X6_3t5UVTZsrprqBQ8NacOV2AQ3vpawt62vBbc8dqyWoRvVK2a53wikYRN8hmk5IHLjiO_Ju0300fjD-oB_CEn1x1Oenp04XVZTAoPxnR95vyDmG8-JS1tOYrDudjHdhSRqbFhuFAqFAcYPaGFKKbtBzHCcTf2sEvQahtyB0EddrEBoLh22cNK9vcvHfJf8jvX02OgZ_OBfeXycpm4YJyVr-B6fFlXA</recordid><startdate>20160401</startdate><enddate>20160401</enddate><creator>周立波 李斐 朱金焕 邹捍 马舒坡 李鹏</creator><general>The Chinese Meteorological Society</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20160401</creationdate><title>Vertical Structures of Atmospheric Properties in Southeast Tibet during the South Asian Summer Monsoon in 2013</title><author>周立波 李斐 朱金焕 邹捍 马舒坡 李鹏</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c489t-27bf308290e2094083d665c2d543cd3e2560787d77cbde4e70f4db11ab461f373</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Atmospheric Sciences</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geophysics and Environmental Physics</topic><topic>Meteorology</topic><topic>南亚夏季风</topic><topic>垂直结构</topic><topic>大气参数</topic><topic>季风期</topic><topic>对流层顶</topic><topic>性质</topic><topic>水分条件</topic><topic>西藏东南部</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>周立波 李斐 朱金焕 邹捍 马舒坡 李鹏</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>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living 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Sinica</addtitle><date>2016-04-01</date><risdate>2016</risdate><volume>30</volume><issue>2</issue><spage>258</spage><epage>264</epage><pages>258-264</pages><issn>2095-6037</issn><issn>0894-0525</issn><eissn>2198-0934</eissn><eissn>2191-4788</eissn><abstract>In June 2013,a field experiment was conducted in Southeast Tibet in which the air temperature,moisture,and wind were measured by using a GPS sounding system.In the present study,based on these observations and ERA-Interim reanalysis data,the vertical structures of these atmospheric properties and the possible influence of the South Asian summer monsoon（SASM） were investigated.On average,the temperature had a lapse rate of 6.8℃ km~（-1） below the tropopause of 18.0 km.A strong moisture inversion occurred at the near-surface,with a strength of 1.7 g kg~（-1）（100 m）~（-1） for specific humidity.During the observation period,the SASM experienced a south phase and a north phase in the middle and by the end of June,respectively.The monsoon＇s evolution led to large changes in convection and circulation over Southeast Tibet,which further affected the local thermal,moisture,and circulation conditions.The strong convection resulted in an elevated tropopause height over Southeast Tibet during the north phase of the SASM,and the large-scale warm and wet air masses delivered by the monsoon caused high local temperature and moisture conditions.</abstract><cop>Beijing</cop><pub>The Chinese Meteorological Society</pub><doi>10.1007/s13351-016-5095-1</doi><tpages>7</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric Sciences Earth and Environmental Science Earth Sciences Geophysics and Environmental Physics Meteorology 南亚夏季风 垂直结构 大气参数 季风期 对流层顶 性质 水分条件 西藏东南部 |
| title | Vertical Structures of Atmospheric Properties in Southeast Tibet during the South Asian Summer Monsoon in 2013 |
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