Volume 41 Issue 4
Jul.  2021
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Article Contents
CHEN Tao, LI Lei, LI Wen, TI Shuo, WU Han, WANG Shihan, LI Renkang, LUO Fushan, ZHANG Huawei, SUN Hailong, SU Jianfeng, LUO Jing, WEI Feng, XU Qingchen, ZENG Chen, HE Zhaohai, DONG Wei, WANG Naiquan. Characteristics of the Atmospheric Electric Field Distribution with Height in Qaidam Basin of Qinghai Province[J]. Chinese Journal of Space Science, 2021, 41(4): 626-634. doi: 10.11728/cjss2021.04.626
Citation: CHEN Tao, LI Lei, LI Wen, TI Shuo, WU Han, WANG Shihan, LI Renkang, LUO Fushan, ZHANG Huawei, SUN Hailong, SU Jianfeng, LUO Jing, WEI Feng, XU Qingchen, ZENG Chen, HE Zhaohai, DONG Wei, WANG Naiquan. Characteristics of the Atmospheric Electric Field Distribution with Height in Qaidam Basin of Qinghai Province[J]. Chinese Journal of Space Science, 2021, 41(4): 626-634. doi: 10.11728/cjss2021.04.626

Characteristics of the Atmospheric Electric Field Distribution with Height in Qaidam Basin of Qinghai Province

doi: 10.11728/cjss2021.04.626 cstr: 32142.14.cjss2021.04.626
  • Received Date: 2020-03-06
  • Rev Recd Date: 2021-01-21
  • Publish Date: 2021-07-15
  • The intensity of atmospheric electric field is an important parameter of atmospheric electricity. Accurate measurements of atmospheric electric field and the analysis of its spatial and temporal characteristics are of great significance to study space weather activities, meteorological activities and geological activities. In the morning of August 26 and 28, the ballooning experiments with atmospheric electric field detector were done by Honghu Project of Chinese Academy of Science in Da Qaidam region of Qaidam Basin, Qinghai Province. By using cross-correlation function method and Principal Component Analysis (PCA) to analyze the data from the mill electric field instruments aboard the balloons respectively, it is demonstrated that although height is the main factor determining the strength of vertical atmospheric electric field, wind also has significant effect on the strength of the atmospheric electric field in this area. Under fair-weather conditions, the absence of thin clouds has some influence on the measurement of atmospheric electric fields. When there are clouds, the speed of wind will indirectly affect the atmospheric electric fields by affecting the formation of clouds. In addition, there is an atmospheric electric field boundary layer in the Qaidam Basin susceptible to the underlying surface. The thickness of this boundary layer is more than 3 kilometers. The changes in the atmospheric electric field in the boundary layer and the distribution of the atmospheric electric field above 3600m were analyzed and fitted when there were no clouds under fair-weather conditions.

     

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