%0 Dataset
%T Daily Hydrological Observation Data of Tangguladongkemadi Glacier Base Camp in 2009
%J National Cryosphere Desert Data Center
%I National Cryosphere Desert Data Center(www.ncdc.ac.cn)
%U http://www.ncdc.ac.cn/portal/metadata/8e2860e9-f9fe-4d3e-8c92-23fc716f508f
%W NCDC
%R 10.12072/ncdc.tacos.db2969.2023
%A He xiaobo
%K Runoff;Meteorological Hydrology;Hydrology
%X Dongkemadi Glacier, located in Tanggula Mountain, is a continental glacier. This glacier is a compound valley glacier formed by the confluence of a southbound main glacier (also known as the Great Winter Kemadi Glacier) and a southwest facing branch glacier (also known as the Little Winter Kemadi Glacier). The main glacier has an area of 14.63 square kilometers, a length of 5.4 km, an elevation of 5275m at the end, and a branch glacier has an area of 1.767 square kilometers, a length of about 2.8 km. Material balance observations have been conducted on the branch glaciers in the past. This dataset is the daily runoff data obtained from Tanggula Dongkemadi Glacier from June 1, 2009 to October 1, 2009