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xi kun lun shan nan po guo zha bing chuan shui wen te zheng de fen xi
Author(s): 
Pages: 582-589
Year: Issue:  4
Journal: Journal of Glaciology and Geocryology

Keyword:  降水量年径流量年平均气温;
Abstract: 郭扎冰川作用区冰川融水径流占流域年径流量的80%。纯冰川融水径流模数为17.7L/s·km~2,冰川融水径流深为200.2mm,冰川消融深是目前我国有实测资料冰川中的最低值。冰川融水径流年内分配很不均匀,夏季(6—8月)占80%,最大消融期为7—9月,占86.3%。
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