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《Chinese Journal of Atmospheric Sciences》 1993-01
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On the Profiles of Wind and Temperature in the Tower Layer

Zhao Ming(Department of Atmospheric Sciences, Nanjing University, Nanjing 210008)  
In this paper, Zilitinkevich 's work on the wind and temperature profiles of the PBL is improved and the reasonable wind and temperature profiles in the tower layer are obtained dynamically. The expression of the height of the PBL under unstable condition is also derived approximately. The wind and temperature profiles can thus be applied to different stratifications. We can calculate the wind and temperature distributions as long as the fluxes in the surface layer are calculated from the surface wind and temperature based on the surface layer theory. The data from the 325m tower in Beijing show that these profiles have attained a fairly high accuracy.
【Fund】: 国家自然科学基金
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【Secondary References】
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1 LI Zhenjie1,2,HE Qing1,Ali Mamtimin1(1.Institute of Desert Meteorology,CMA,Urumqi 830002,China;2.College of Geographical Science and Tourism,Xinjiang Normal University,Urumqi 830054,China);Preliminary Summary of Studies on Characteristics of Atmospheric Turbulent Energy Exchange Near Surface Layer of Arid Desert Area[J];Journal of Arid Meteorology;2009-02
2 LI Xiaolan1,2,ZHANG Hongsheng1 (1.Department of Atmospheric and Oceanic Sciences,School of Physics,Peking University,Beijing 100871,China;2.Key Laboratory for Semi-Arid Climate Change of the Ministry of Education,Lanzhou University,Lanzhou 730000,China);Review on Characteristics of Micrometeorology and Turbulent Transfer During Dust Events in China[J];Journal of Arid Meteorology;2010-03
3 Fan Bin(Inner Mongolia Meteorological Observatory,Hohhot 010051);Preliminary Study on the Influence of the Yinshan Mountains to the Meteorological Elements of the Central Region of the Inner Mongolia[J];Meteorology Journal of Inner Mongolia;2010-01
4 KANG Ling1,SUN Xin1,HOU Ting1,SHEN Jian-guo2,GUO Rui-qing3(1.Inner Mongolian Meteorological Station,Hohhot 010051,China;2.Shandong Province Meteorological Bureau,Jinan 250031,China;3.Inner Mongolian Ecology and Agriculture Weather Center,Hohhot 010051,China);Distribution Characteristics of Sandstorms in Inner Mongolian Area[J];Journal of Desert Research;2010-02
5 HE Qing1,2, LIU Qiang1,2,3, YANG Xing-hua1,2, Ali Mamtimin1,2, HUO Wen1,2, LIANG Yun1,2(1.Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China; 2.Taklimakan Desert Atmosphere and Environment Observation and Experiment Station, Tazhong 841000, Xinjiang, China; 3.College of Resources and Environmental Science, Xinjiang University, Urumqi 830046, China);Profiles of Atmosphere Boundary Layer Ozone in Winter over Hinterland of Taklimakan Desert[J];Journal of Desert Research;2010-04
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1 Kang Ling 1 Sun Xin 1 Hou Ting 1 Shen Jianguo 2 Guo Ruiqing 3(1.Inner Mongolian Meteorological Station,Huhhot 010051,China;2.Shandong Province meteorological bureau,Jinan 250031,China;3.Inner Mongolian ecology and agriculture weather center,Huhhot 010051,China);Distribution characteristic Analysis of Sandstorm in Inner Mongolian Area[A];[C];2010
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