The relationship among summer atmospheric boundary layer height over the Taklimakan Desert, its land surface parameters and Eurasian circulation-Reference-Cited by-同舟云学术

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The relationship among summer atmospheric boundary layer height over the Taklimakan Desert, its land surface parameters and Eurasian circulation

Published:2022-07-27 Issue:11 Volume:23 Page:
ISSN:1530-261X
Container-title:Atmospheric Science Letters
language:en
Short-container-title:Atmospheric Science Letters

Author:

Wang Minzhong¹²³⁴^ORCID,Zhang Jiantao¹²³⁴

Affiliation:

1. Institute of Desert Meteorology, China Meteorological Administration Urumqi China

2. National observation and Research Station of Desert Meteorology, Taklimakan Desert of Xinjiang Urumqi China

3. Taklimakan Desert Meteorology Field Experiment Station of China Meteorological Administration Urumqi China

4. Xinjiang Key Laboratory of Desert Meteorology and Sandstorm Urumqi China

Publisher

Wiley

Subject

Atmospheric Science

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/asl.1122

Reference32 articles.

1. Summer boundary-layer height at the plateau site of Dome’C, antarctica

2. Reasons for the Extremely High-Ranging Planetary Boundary Layer over the Western Tibetan Plateau in Winter

3. He Q.(2009)Observation study of atmospheric boundary layer structure and land atmosphere interaction in the Tazhong of Taklimakan Desert. PhD Dissertation. Nanjing: Nanjing University of Information Science & Technology 80–100.

4. Global radiation characteristics and influencing factors of Taklimakan Desert hinterland;He Q.;Journal of Desert Research,2008

5. Characteristic of long wave radiation over the Taklimakan Desert hinterland;He Q.;Plateau Meteorology,2009

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