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glacier response
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     1 Glacier.
     研究区域主要集中于1号冰川及其邻近地区。
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     Glacier Club
     冰河高尔夫俱乐部
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     evaluation and response;
     评价与反馈;
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     On Compliment and Response
     论赞扬语及应答
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     Variations of Glacier Mass Balance and Their Response to Climatic Change
     近40年来冰川物质平衡变化及对气候变化的响应
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  glacier response
The later shrinkage is attributed to the glacier response to the air temperature rise in region.
      
The glacier response to climate changes is not only measured by mass-balance calculations but by changes in their front position and dynamics.
      
This is important for understanding the nature of glacier response to climate variability and its circulation.
      
Nevertheless, GPS observations provided significant information about the glacier response to tidal forcing.
      


Most of the mountain glaciers in the Northern Hemisphere are retreating recently because of the negative mass balance, reflecting the warm tendency of the climate change. The glacier mass balance in the mountains of the Northern Hemisphere has a significant regional features owing to the difference of the regional climate variations and the glacier responses to climate changing.

近期北半球大多数山地冰川的物质平衡为负,冰川普遍退缩,表明北半球气候暖化的趋势.由于区域气候波动和变化的差异性以及冰川对气候变化的敏感性(响应程度)的不同,北半球山地冰川在普遍退缩的背景下具有鲜明的区域特征.

During the Sino-American Expedition to Mt. Qomolangma in 1997, the Rongbuk Glacier was investigated and its terminus location was measured by means of GPS techniques. Comparison with 1966′s measurement yields that in the past 30 years the glacier has retreated 170~270 m, equivalent to a retreat speed of 5 5~8 7 m/a. This suggests that climate in the region has mainly been in warming since the early part of this century, because glacier response to climatic change has a retardation. Due to climatic still...

During the Sino-American Expedition to Mt. Qomolangma in 1997, the Rongbuk Glacier was investigated and its terminus location was measured by means of GPS techniques. Comparison with 1966′s measurement yields that in the past 30 years the glacier has retreated 170~270 m, equivalent to a retreat speed of 5 5~8 7 m/a. This suggests that climate in the region has mainly been in warming since the early part of this century, because glacier response to climatic change has a retardation. Due to climatic still warming in recent ten years, the glacier retreat will continue for several decades.

997年中美联合考察队对珠穆朗玛峰绒布冰川考察期间,采用GPS技术对冰川末端位置进行了测量.将其结果与1966年考察测量的位置对比得出,过去30a间该冰川末端后退了170~270m,平均年退缩量为55~87m.由于目前气候仍在变暖,该冰川将继续保持退缩状态.

 
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