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横断山区垂直气候的几个问题
张谊光
1998
Source Publication资源科学
ISSN1007-7588
Volume020Issue:003Pages:12
Abstract根据云岭白马雪山3a多的垂直气候观测资料分析,气温垂直递减率比一般地区大,西坡为0.71℃/100m,东坡达0.78℃/100m;在一定海拔高度范围内,降水量随高度升高而增加,在“三江”最狭窄的平行岭谷地段,最大降水高度出现在背风坡(东坡)上部海拔3700 ̄3800之间,风对降水量的影响显著,风口处的降水量比非风口处的观测场内少8% ̄12%。
Language英语
Document Type期刊论文
Identifierhttp://ir.igsnrr.ac.cn/handle/311030/119538
Collection中国科学院地理科学与资源研究所
Affiliation中国科学院地理科学与资源研究所
First Author Affilication中国科学院地理科学与资源研究所
Recommended Citation
GB/T 7714
张谊光. 横断山区垂直气候的几个问题[J]. 资源科学,1998,020(003):12.
APA 张谊光.(1998).横断山区垂直气候的几个问题.资源科学,020(003),12.
MLA 张谊光."横断山区垂直气候的几个问题".资源科学 020.003(1998):12.
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