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An investigation into the vertical structures of low‐altitude atmosphere over the Central Taklimakan Desert in summer

机译：夏季中央塔克拉曼沙漠沙漠中低空大气垂直结构的调查

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Jinfang Yin; Haodong Gu; Jie Huang; Minzhong Wang;
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1. Vertical distribution of dust in the Martian atmosphere during northern spring and summer: High-altitude tropical dust maximum at northern summer solstice [J] . N. G. Heavens, M. I. Richardson, A. KleinbOh, Journal of geophysical research. Planets . 2011,第E1期

机译：春季和夏季北部火星大气中粉尘的垂直分布：夏至北部高空热带尘埃最多
2. Observational study of formation mechanism, vertical structure, and dust emission of dust devils over the Taklimakan Desert, China [J] . Chong Liu, Tianliang Zhao, Xinghua Yang, Journal of Geophysical Research, D. Atmospheres: JGR . 2016,第7期

机译：塔克拉玛干沙漠上空沙尘暴的形成机理，垂向结构及扬尘的观测研究
3. Impacts of Irrigation and Vegetation Growth on Summer Rainfall in the Taklimakan Desert [J] . Dongze XU, Yanluan LIN 大气科学进展（英文版） . 2021,第011期

机译：Impacts of Irrigation and Vegetation Growth on Summer Rainfall in the Taklimakan Desert
4. Regional variation of fine particle number in soil around the ground surface in central and western part of the Taklimakan Desert [C] . Osamu Abe, Kenji Kosugi, Junrong Xu, ADEC Workshop . 2005

机译：塔克拉玛山沙漠中部和西部地面围绕地面围绕地面细粒子数的区域变异
5. Vertical tritium transport from the shallow unsaturated zone to the atmosphere, Amargosa Desert Research Site, Nevada. [D] . Garcia, Christina Amanda. 2007

机译：内华达州阿马戈萨沙漠研究中心的垂直tri运输从浅层不饱和带到大气。
6. Characteristics of land-atmosphere interaction parameters in hinterland of the Taklimakan Desert [O] . Yongqiang Liu, Xianyong Meng, Ali Mamtimin, -1

机译：塔克拉玛干沙漠腹地的陆-气相互作用参数特征
7. Observational study of formation mechanism, vertical structure, and dust emission of dust devils over the Taklimakan Desert, China [O] . Chong Liu, Tianliang Zhao, Xinghua Yang, 2016

机译：中国塔克拉曼沙漠尘埃魔法污秽的形成机制，垂直结构和尘埃发射的观察研究
8. Bacterial Flux from Chaparral into the Atmosphere in Mid-Summer at a High Desert Location [R] . Lighthart, R., Shaffer, B. T. 1994

机译：夏季中部高沙漠地区的Chaparral细菌通量

An investigation into the vertical structures of low‐altitude atmosphere over the Central Taklimakan Desert in summer

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