The atmosphere turbidity Coefficient of Yunling Baimang Snow Mountain in the central part of the Hengduan Mountain Range
Article
Figures
Metrics
Preview PDF
Reference
Related
Cited by
Materials
Abstract:
According to the data of solar direct radiation observation at the Yunling Bai-mang Snow Mountain in the cenTRal part of the Hengduan Mountain Range in 1983 and 1984,the Linke atmosphere turbidity coefficient TP was calculated and analysed. It's found that TP decreases with the increase of altitude. The annual variations of TP show similar TRend at different altitude.TP is maximum in July and August, and TP is Minimum in November. TP may he divided into the aerosol turbidity coefficient TR and the vapour turbidity coefficient TW, The annual variation of TW is in accordance with the annual disTRibution of the precipitation, and TR shows the opposite variation tendency.