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Characteristics of the atmospheric boundary layer's structure and heating (cooling) rate in summer over the Northern Tibetan Plateau.

Authors :
Gu, Lianglei
Yao, Jimin
Hu, Zeyong
Ma, Yaoming
Sun, Fanglin
Yu, Haipeng
Wang, Shujing
Yang, Yaoxian
Guo, Ruixia
Qin, Yanyan
Source :
Atmospheric Research. May2022, Vol. 269, pN.PAG-N.PAG. 1p.
Publication Year :
2022

Abstract

The atmospheric boundary layer (ABL) is one of the most fundamental yet complex components of the Earth's atmosphere. Hence, studying the ABL has important theoretical value and practical significance. In this paper, the structural characteristics and heating (cooling) rate of the ABL in summer over the Northern Tibetan Plateau (NTP) were analysed using radiosonde observation data from the Amdo and Nagqu regions. The results indicate that the summertime ABL height over the NTP exhibited obvious diurnal variations, with the ABL height during the dry season being greater than that during the rainy season. The maximum convective boundary layer (CBL) height during the daytime reached 3200 m and 2500 m in the dry and rainy seasons, respectively, and the mean maximum CBL height was approximately 2500 m; the maximum stable boundary layer (SBL) height at night reached 900 m, and the mean maximum SBL height was approximately 500 m. The wind speed dominated by westerly wind in the dry season was greater than that dominated by easterly wind in the rainy season, and the zonal (meridional) wind speed (shear) on sunny days was greater than that on cloudy days. The inverse humidity phenomenon occurred in both Amdo and Nagqu, and the strong humidity inversion occurred mainly at midnight on sunny days and at noon on cloudy days. The heating (cooling) rate of the ABL displayed obvious diurnal variations, with the rates being greater on sunny days and lower on cloudy and rainy days. Furthermore, the mean values of the daytime heating rate and nighttime cooling rate of the ABL were relatively equal, indicating that the atmospheric energy budget was, for the most part, balanced. • The ABL height in summer over the Northern Tibetan Plateau was determined. • The heating and cooling rates of the ABL in summer were calculated. • The wind speed (shear) in the dry season was greater than that in the rainy season. • The inverse humidity phenomenon occurred at both Amdo and Nagqu. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
01698095
Volume :
269
Database :
Academic Search Index
Journal :
Atmospheric Research
Publication Type :
Academic Journal
Accession number :
155455851
Full Text :
https://doi.org/10.1016/j.atmosres.2022.106045