1982年8月—1983年7月拉萨、那曲、改则、甘孜地面热量平衡分析

THE HEAT BALANCE IN THE LHASA, NAGQU, GÊRZÊ AND GARZÊ DURING AUGUST1982 TO JULY 1983

摘要: 本文用1982年8月1日至1983年7月31日青藏高原热源观测资料1,依据相似性理论,用通量—廓线关系计算了拉萨、那曲、改则、甘孜四站的感热和潜热通量值,辐射平衡用实测值,地表热通量则由5,10cm深度的土壤热通量外推得到2。从而得到上述4站的地面热源强度。

Abstract: Based on the theory of a similarity and the wind, temperature, hymidity profile data observed in the 1982-1983 plateau's heat source investigation, the Dyer and Hicks Fluxprofile Relationships have been used to evaluate the tomponents of the heat balance and the intensity of the heat source for stations Lhasa, Nagqu, Gêrzê, Garzê.