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A multi-location joint field observation of the stratosphere and troposphere over the Tibetan Plateau

查看全文 作  者:JinQiang [1,2,3]Zhang;Yi [1,3]Liu;HongBin [1,2,3]Chen;ZhaoNan [1,3]Cai;ZhiXuan [1,3]Bai;LingKun [4]Ran;Tao [5]Luo;Jing [1,2,3]Yang;YiNan [1]Wang;YueJian [1]Xuan;YinBo [5,6]Huang;XiaoQing [5,6]Wu;JianChun [1,3]Bian;DaRen [1,3]Lu 高影响力作者 机构地区:[1]Key Laboratory of Middle Atmosphere and Global Environment Observation, Institute of Atmospheric Physics, Chinese Academy of Sciences;[2]Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology;[3]University of Chinese Academy of Sciences;[4]Key Laboratory of Cloud-Precipitation Physics and Severe Storms, Institute of Atmospheric Physics, Chinese Academy of Sciences;[5]Key Laboratory of Atmospheric Optics, Anhui institute of optics and Fine Mechanics, Chinese Academy of Science;[6]Science Island Branch of Graduate School, University of Science and Technology of China高影响力机构 出  处:《Earth and Planetary Physics》索引2019年第3卷第2期,共6页高影响力期刊 基  金:supported by the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant Nos. XDA17010101, XDA17010102, XDA17010103, XDA17010104 and XDA17010105) 摘  要:The unique geographical location and high altitude of the Tibetan Plateau can greatly influence regional weather and climate.In particular, the Asian summer monsoon(ASM) anticyclone circulation system over the Tibetan Plateau is recognized to be a significant transport pathway for water vapor and pollutants to enter the stratosphere. To improve understanding of these physical processes, a multi-location joint atmospheric experiment was performed over the Tibetan Plateau from late July to August in 2018, funded by the fiveyear(2018–2022) STEAM(stratosphere and troposphere exchange experiment during ASM) project, during which multiple platforms/instruments—including long-duration stratospheric balloons, dropsondes, unmanned aerial vehicles, special sounding systems, and ground-based and satellite-borne instruments—will be deployed. These complementary methods of data acquisition are expected to provide comprehensive atmospheric parameters(aerosol, ozone, water vapor, CO_2, CH_4, CO, temperature, pressure,turbulence, radiation, lightning and wind); the richness of this approach is expected to advance our comprehension of key mechanisms associated with thermal, dynamical, radiative, and chemical transports over the Tibetan Plateau during ASM activity. 关 键 词:TIBETAN PLATEAU Asian summer MONSOON STRATOSPHERE and troposphere exchange
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