它超过180公里(112英里)长，从极地高原(图的左边)一直流到罗斯冰架(图的右边)。
More than 180 kilometers [112 miles] long, the glacier flows down from the polar plateau (left) to the Ross Ice Shelf (right).
文章讨论了末次冰消开始时期青藏高原南部普莫雍错湖芯沉积反映的环境暖湿化以及原因。
This paper revealed a warm and humid environment during the initial stage of the last deglacial period in the Pumoyum Co Lake of the southern Tibet and analyzed several possible reasons.
由于自然、历史、社会等原因，人们对高原冰湖的研究甚少，除险施工更是少之又少。
Due to the natural, historical and social factors, very few studies on ice lake on highland are carried out with even less studies on disaster-relief during construction.
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