Description: K index reflects the stable stratification of the atmosphere, but it can not be expressed clearly unstable atmospheric stratification of the entire layer. From the above equation, A index includes not only the temperature lapse rate between the layers, but also lower, the lower and middle temperature and humidity conditions. A larger index, the atmosphere more unstable, and the more humid.
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7组\500-850\13日18时.jpg
...\.......\5日18时.jpg
...\.......\6日00时.jpg
...\.......\air.dat
...\.......\qes-hr00day6.gmf
...\.......\qes-hr18day13.gmf
...\.......\qes-hr18day5.gmf
...\.......\qes.ctl
...\.......\QES.grd
...\.......\qes2.gs
...\.......\qes500-800inmay.gs
...\.......\qes500-850.gmf
...\.......\Qse.f90
...\.......\rhum.dat
...\.......\说明.txt
...\a.for
...\k.for
...\不稳定诊断.ppt
...\500-850
7组
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