Articles | Volume 24, issue 18
https://doi.org/10.5194/acp-24-10947-2024
https://doi.org/10.5194/acp-24-10947-2024
Measurement report
 | 
27 Sep 2024
Measurement report |  | 27 Sep 2024

Measurement report: The promotion of the low-level jet and thermal effects on the development of the deep convective boundary layer at the southern edge of the Taklimakan Desert

Lian Su, Chunsong Lu, Jinlong Yuan, Xiaofei Wang, Qing He, and Haiyun Xia

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Latest update: 13 Dec 2024
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Short summary
The cold downhill airflow of the Tibetan Plateau leading to the low-level jet weakens the height and intensity of the inversion layer, which reduces the energy demand for the broken inversion layer. The low-level jet causes dust aerosols to accumulate near the ground. The material conditions for the development of the desert atmospheric boundary layer can be quickly transformed into thermal conditions.
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