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青藏高原五道梁地区湍流输送特征的研究
引用本文:祁永强,王介民.青藏高原五道梁地区湍流输送特征的研究[J].高原气象,1996,15(2):172-177.
作者姓名:祁永强  王介民
作者单位:中国科学院兰州高原大气物理研究所
摘    要:根据1994年6-7月在青藏高原五道梁地区的湍流脉动观测资料,分析了该地区近地层能量平衡、感热和谱热的日变化及湍流强度和端流谱特征。结果表明:晴天该地区近地层能量基本平衡,各能量分量的日变化与常情况相同;白天感热通量的输送占主导地位,潜热通量占次要地位,符合半干旱的一般特征。

关 键 词:青藏高原  近地面层  能量平衡  湍流通量  湍流谱

A STUDY OF TURBULENT TRANSFER CHARACTERISTICS IN WUDAOLIANG AREA OF QINGHAI-XIZANG PLATEAU
Qi Yongqiang,Wang Jiemin,Jia Li Liu Wei,Ma Yaoming,Ren Yanxia.A STUDY OF TURBULENT TRANSFER CHARACTERISTICS IN WUDAOLIANG AREA OF QINGHAI-XIZANG PLATEAU[J].Plateau Meteorology,1996,15(2):172-177.
Authors:Qi Yongqiang  Wang Jiemin  Jia Li Liu Wei  Ma Yaoming  Ren Yanxia
Abstract:The paper analyses the turbulent data ,which collected from the Wudaoliang area of Qinghai-Xizang Plateau in June July 1994. The results show:in the area,the energy fluxes of surface layer can approximately balance. The diurnal variations of net radiation,sensible heat,latent heat and ground heat flux are normal. The sensible heat flux is dominant,the latent heat flux is second in energy balance. Spectra of wind component analysis show,in near neutral stability,the vertical velocity spectral peak is about f=0.3,it is good when compared with others,but the longitudinal velocity (u spectrum) peak is about f=0.1,the cross velocity (v spectrum ) is about f=0.2,which are higher than other results. There are same results in vertical velocity spectrum compared with other results.
Keywords:Qinghai-Xizang Plateau  Surface layer  Energy budget  Turbulent flux  Turbulent spectrum
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