高原冰川

东帕米尔高原冰川花岗岩漂砾风化穴初步研究

A preliminary study on Tafoni developed on glacial granite boulders in Eastern Pamir

青藏高原冰川融化引起的均衡上升运动与构造力引起的结果相比是非常微弱和从属的，并属后期阶段。

Isostatic ascending motion , which was resulted from the glacial dissolve of the Qinghai Tebet plateau , is much weaker and Less important than that of the structure force and it belongs the later period stage .

该报告同时还警告说青藏高原的冰川正在迅速融化。

The report also warns of rapidly melting glaciers .

季风亚洲末次冰期可统一称为大理冰期，古冰川首次出现于东亚海岸山地，内陆高山高原则冰川规模缩小。

On the whole , the Last Glaciation in monsoonal Asia should be termed as the Dali Glaciation which is quite in accord with the Zyryanka Glaciation in Northeast Asia .

青藏高原内陆水系各冰川系统的结构特征及变化趋势预测

The Structure Characteristics and Variation Prediction of Glacier Systems in Qinghai-Xizang Plateau Interior Area

结果，高原上82%的冰川都在退缩，而10%的永久冻土带正在退化。

As a result , 82 per cent of the plateau 's glaciers have retreated while ten per cent of its permafrost has degraded .

与谢自楚、冯清华、王欣及笔者对中国其它冰川系统的预测结果进行比较，结果显示：青藏高原内陆水系各冰川系统敏感性小，稳定性大。

Comparing with other glacier systems in other regions of China , Glacier Systems in Qinghai-Xizang Plateau Interior Area has small sensitivity and big stabilization .

根据中国科学院寒区旱区环境与工程研究所冰川目录数据库的资料，利用物质平衡与冰川系统理论，统计分析了青藏高原内陆水系各冰川系统的规模结构、高度结构。

Based on the Glacier Inventory Database of Cold and Arid Regions Environmental and Research Institute , the article used the theory of mass balance and glacier system , calculated and analyzed the scale structure and the altitude structure of Glacier Systems in Qinghai-Xizang Plateau Interior Area .

南亚排放的黑碳可能抵达青藏高原南部腹地，对青藏高原的冰川表面能量平衡有一定影响。

BC emitted from South Asia could penetrate into the inland of TP and might have significant effects on the surface energy balance of the glaciers in the TP .