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希夏邦马峰抗物热冰川区消融期气候特征
引用本文:刘时银,谢自楚,马力.希夏邦马峰抗物热冰川区消融期气候特征[J].冰川冻土,1996(3).
作者姓名:刘时银  谢自楚  马力
作者单位:中国科学院兰州冰川冻土研究所,新疆维吾尔自治区气象科学研究所,乌鲁木齐
摘    要:根据1993年夏季在希夏邦马峰抗物热冰川考察时取得的部分气象要素观测资料,结果表明,尽管夏季气温相对较高,但由于降水频繁,冰川表面降雪,通过增加冰面反射,削弱冰面消融,导致冰川水文循环水平低。温度观测揭示出受西南季风影响,夏季冰川区处于高温环境中;又由于相对远离主山脉,且无明显的山谷形态,该冰川区局地环流不发育,整个观测期间均受制于东南和南风控制之下

关 键 词:抗物热冰川  气温  降水局  地环流

Characteristics of Summer Climate in the Area of Kangwure Glacier, Xixiabangma Mt.
Liu Shiyin ,Xie Zichu and Ma Li.Characteristics of Summer Climate in the Area of Kangwure Glacier, Xixiabangma Mt.[J].Journal of Glaciology and Geocryology,1996(3).
Authors:Liu Shiyin  Xie Zichu and Ma Li
Institution:Liu Shiyin 1,Xie Zichu 1 and Ma Li 2
Abstract:Based on the meteorological observation during the summer, 1993, the general characteristics of air temperature, precipitation, and wind direction and speed on Kangwure Glacier are discussed in the present paper. Observations demonstrate that frequent snowfall on the glacier surface makes ablation process weakened by increasing the surface albedo though summer temperature is higher over the glacier. The observed relative humidity reveals that this glacier is influenced by prevailed air mass with higher moisture from Indian ocean monsoon in the summer. Away from the main range of Mt. Xixiabangma and without clear incised valley, local circulation is insignificant and the whole glacier were covered by southerly and southeasterly.
Keywords:Kangwure Glacier    temperature    precipitation  local circulation
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