Discharge Data at the outlet of the Tsho Rolpa Glacial Lake, Rolwaling Himal, Nepal Himarayas (WLD-TR).

These data, for understanding the hydro-meteorological environment, taken as the basis for the study of development and formation process of Tsho Rolpa glacier lake. Tsho RoIpa galcier Lake（27o51’N, 86o29'E）is located at 110km east-north of Kathmandu and developed on the terminus of the Trakarding Glacier (or Lower Trambau Glacier), Rolwaling Valley, eastern Nepal. The drainage area including the lake surface is 77.6km2 with the 71.8% glacier coverage; 55.3% and 16.5% are occupied by debris-free and debris-covered glacier, respectively (Yamada, 1996).the lake surface area and volume were 1.39 km2 and 77.6 million m3 in 1994, respectively(Kadota, 1994). The instrument install to outlet of Glacier lake terminus.本数据集旨在支撑水文气象环境相关研究，同时作为措罗帕冰川湖（Tsho Rolpa Glacier Lake）发育与形成过程研究的基础数据。措罗帕冰川湖（地理坐标为北纬27°51′、东经86°29′）地处尼泊尔东部罗尔瓦林谷，距加德满都东偏北110千米，发育于特拉卡丁冰川（亦称下特兰博冰川，Trakarding Glacier/Lower Trambau Glacier）的末端区域。该流域（含湖面）总面积达77.6平方千米，冰川覆盖率为71.8%；其中无碛冰川（debris-free glacier）与有碛冰川（debris-covered glacier）占比分别为55.3%与16.5%（Yamada，1996）。1994年，该冰川湖的湖面面积与容积分别为1.39平方千米与7760万立方米（Kadota，1994）。监测设备已布设至该冰川湖末端的出水口处。