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托木尔峰地区的冰川气象

GLACIAL METEOROLOGY ON MT. TUOMUER

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【作者】 寇有观; 丁良福; 李文忠; 张永亮;

【Author】 Kou youguan, Ding Liangfu, Li Wengzhong, Zhang yongling ( Lanzhou Institute of Glaciology and Cryopedology, Academia Sinica )

【机构】 中国科学院兰州冰川冻土研究所; 中国科学院兰州冰川冻土研究所;

【摘要】 <正>托木尔峰登山科学考察中,冰川气象组在西琼台兰冰川区开展了一系列气象观测,对温度、降水、辐射、小气候、热平衡进行了考察研究。其基本观测点设在西琼台兰冰川侧碛上(80°17′E,41°45′N,海拔高度3200米)。同时,在3400米的冰川表碛上安装了百叶箱,设置温、湿度的自记仪器。在4000米高度上分设冰面和表碛两个观

【Abstract】 In July 1978 the precipitation increased in the Mt. Tuomuer area as compared with the region outside of it. At the forest zone, about 2400m a. s.l., in Mt. Tuomuer area appears the first height of maximum precipitation, from this zone upwards, the precipitation decrea-ses; but up to 3200 m a. s. 1. the precipitation increases aed exceeds that at 2400 m a. s. 1. At 3900-4000 m a. s.l., the precipitation increases continuously, being 127.7% of that at 3200 m a.s.l. The area at about 5250 m a. s 1. is the second height of maximum precipitation with annual precipitation reaching about 900 mm, which provides an enough mass source for glacier development.Of the total heat input to the glacier surface, the radiation balance takes about 60%, sensible heat about 40%. Both of which are large enough for the heating source of strong glacier ablation.

  • 【文献出处】 冰川冻土 ,Journal of Glaciology and Geocryology , 编辑部邮箱 ,1980年04期
  • 【被引频次】4
  • 【下载频次】72
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