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Why Are There More Summer Afternoon Low Clouds Over the Tibetan Plateau Compared to Eastern China?
Author(s) -
Wang Yinjun,
Zeng Xubin,
Xu Xiangde,
Welty Joshua,
Lenschow Donald H.,
Zhou Mingyu,
Zhao Yang
Publication year - 2020
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2020gl089665
Subject(s) - plateau (mathematics) , environmental science , relative humidity , cloud cover , atmospheric sciences , climatology , daytime , sensible heat , boundary layer , planetary boundary layer , flux (metallurgy) , humidity , turbulence , meteorology , geology , geography , cloud computing , materials science , physics , mathematical analysis , mathematics , computer science , thermodynamics , operating system , metallurgy
In this study, we analyze the relationships between summer afternoon low cloud cover and environmental conditions over the Tibetan Plateau (TP). Using in situ measurements, satellite data, and reanalysis, and based on theoretical analysis, we find that there is stronger thermal turbulence, lower temperature, and higher frequency of low cloud formation for the same surface relative humidity over the eastern and central TP compared with eastern China. With the same sensible heat flux, decreased air density enhances buoyancy flux, which increases the planetary boundary layer height and moisture vertical transport. At the same time, with the same near‐surface relative humidity, lower temperature over the TP decreases the lifting condensation level, which increases the probability of the air parcel reaching this level. Compared to the low‐elevation region in eastern China, these two mechanisms enhance low cloud occurrence in the afternoon over the TP.