Diurnal variations of turbulence parameters over the tropical oceanic upper troposphere during SCSMEX

作     者：LIU Xiao XU JiYao YUAN Wei 

作者机构：State Key Laboratory of Space Weather Center for Space Science and Applied ResearchChinese Academy of Sciences College of Mathematics and Information Science Henan Normal University 

出 版 物：《Science China(Technological Sciences)》 (中国科学（技术科学英文版）)

年 卷 期：2014年第57卷第2期

页      面：351-359页

核心收录：

学科分类：07[理学] 070601[理学-气象学] 070602[理学-大气物理学与大气环境] 0706[理学-大气科学] 

基　　金：supported by Chinese Academy of Sciences(Grant No.KZZD-EW-01-2) the National Natural Science Foundation of China(Grant Nos.41004063,41374158,41229001 and 41331069) the National Basic Research Program of China(Grant No.2011CB811405) supported in part by the Specialized Research Fund and the Open Research Program of the State Key Laboratory of Space Weather 

主　　题：diurnal variation turbulence tropical troposphere mesoscale convection systems 

摘      要：Using the method of Thorpe analysis, the TKE （turbulence kinematic energy） dissipation rate （e） and turbulence diffusivity （K） were derived from the RS （radiosounding） measurements in the tropical oceanic upper troposphere. The measurements were performed four times per day during two intense observation periods （May 5-25, and June 5-25） on the Kexue #1 scientific observation ship of SCSMEX （South China Sea Monsoon EXperiment） in 1998. There are three new features obtained from our analysis. First, the responses of e and K to the onset of monsoon are negligible over the ocean at least for the data used here Second, the temporal variations of e and K are in a similar manner and exhibit strong diurnal variations. The diurnal variations achieve their maxima in the morning （08 LT） and early afternoon （14 LT）, and achieve their minima in the evening （20 LT） and early morning hours （02 LT）. The diurnal variations of turbulence parameters （e and K） and their responses to the onset of monsoon are entirely different from those derived over land at similar latitudes. Finally, although the correlations between the variations of e and MCSs （mesoscale convective systems）, which were derived from TRMM （tropical rainfall measuring mis- sion） satellite, are not very well in only few days, the diurnal variations of e averaged over May and June are strongly correlat- ed with the diurnal variations of MCSs with correlation factors of 0.79 and 0.94, respectively. This indicates that the turbulence and its diurnal variations over the tropic oceanic upper stratosphere region are highly related to the MCSs.