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Study on Characteristics of Atmospheric Boundary Layer over Naqu Region of Northern Tibetan Plateau

Maoshan Li, Yaoming Ma, Zeyong Hu, Weiqiang Ma, Jiemin Wang, Ogino Shin-Ya

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Abstract

Using the observed data in the PIOP (pre-intensive observing period) of CAMP/Tibet (coordinated enhensive observation period (CEOP) Asian-Australian Monsoon Project (CAMP) in the Tibetan Plateau), the characteristics of daily change of equivalent potential temperature, specific humidity and wind speed, as well as that of the steady and convective boundary layers over Naqu region of northern Tibetan Plateau were analyzed. The results showed that the daily change of boundary layer over Naqu region of northern Tibetan Plateau is significant, the height of convective mixed layer can reach 1800 m, and time forming converctive boundary layer in rain day is later than that in cloudy and fine days.

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What this paper is about

Using the observed data in the PIOP (pre-intensive observing period) of CAMP/Tibet (coordinated enhensive observation period (CEOP) Asian-Australian Monsoon Project (CAMP) in the Tibetan Plateau), the characteristics of daily change of equivalent potential temperature, specific humidity and wind speed, as well as that of the steady and convective boundary layers over Naqu region of northern Tibetan Plateau were analyzed. The results showed that the daily change of boundary layer over Naqu region of northern Tibetan Plateau is significant, the height of convective mixed layer can reach 1800 m, and time forming converctive boundary layer in rain day is later than that in cloudy and fine days.

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Available abstract

Using the observed data in the PIOP (pre-intensive observing period) of CAMP/Tibet (coordinated enhensive observation period (CEOP) Asian-Australian Monsoon Project (CAMP) in the Tibetan Plateau), the characteristics of daily change of equivalent potential temperature, specific humidity and wind speed, as well as that of the steady and convective boundary layers over Naqu region of northern Tibetan Plateau were analyzed. The results showed that the daily change of boundary layer over Naqu region of northern Tibetan Plateau is significant, the height of convective mixed layer can reach 1800 m, and time forming converctive boundary layer in rain day is later than that in cloudy and fine days.

Key concepts: Plateau (mathematics), Climatology, Boundary layer, Monsoon, Atmospheric sciences, Planetary boundary layer, Humidity, Environmental science

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