Volume 42 Issue 3
Jun.  2022
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HU Yaoyue, WANG Donghai, WU Zhenzhen, ZHANG Chunyan, ZENG Zhilin, WAN Yijing. Analysis of the Observational Characteristics of the Quasi-zero Wind Layer in the Near Space over China (in Chinese). Chinese Journal of Space Science, 2022, 42(3): 383-395. DOI: 10.11728/cjss2022.03.210303022
Citation: HU Yaoyue, WANG Donghai, WU Zhenzhen, ZHANG Chunyan, ZENG Zhilin, WAN Yijing. Analysis of the Observational Characteristics of the Quasi-zero Wind Layer in the Near Space over China (in Chinese). Chinese Journal of Space Science, 2022, 42(3): 383-395. DOI: 10.11728/cjss2022.03.210303022

Analysis of the Observational Characteristics of the Quasi-zero Wind Layer in the Near Space over China

doi: 10.11728/cjss2022.03.210303022
  • Received Date: 2021-02-27
  • Accepted Date: 2021-05-21
  • Rev Recd Date: 2022-02-06
  • Available Online: 2022-05-23
  • The Quasi-zero Wind Layer is a transition region with low zonal wind speed in the lower stratosphere, which is important reference for the development and utilization of the near space (20~100 km) and has been attracting worldwide interest. In this paper, the whole country (China) is divided into five regions (15°N-20°N, 20°N-25°N, 25°N-30°N, 30°N-40°N, and 40°N-50°N) based on the L-band radar soundings secondly data of stations from January 2010 to December 2019. The structural characteristics of the Quasi-zero Wind Layer in China and its variations with latitude and season are analyzed. The single/double Quasi-zero Wind Layer is defined according to the different observed wind fields from the data. Results show that the overall distribution of the single/double Quasi-zero Wind Layer in the five regions is generally different distinguished from the separating latitude of 25°N: The single Quasi-zero Wind Layer mainly appears in summer to the north of 25°N. The double Quasi-zero Wind Layer mainly appears to the south of 25°N from October to May of the next year. The average maintenance heights of the single/double Quasi-zero Wind Layer increase with the increasing latitude, and its thickness shows mainly bimodal variation. The occurrence and maintenance days of the single Quasi-zero Wind Layer are more than that of the double Quasi-zero Wind Layer , and the maintenance days in the north of 30°N are significantly prolonged.

     

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