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 p>
collect time | 2009/05/26 - 2009/10/01 |
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collect place | Qinghai Tibet Plateau, Tanggula Mountain, Dongkemadi |
data size | 10.6 KiB |
data format | xlsx |
Coordinate system | WGS84 |
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Automatic collection, manual collection
Professional personnel are responsible for all stages of data acquisition and processing, and the data quality is good p>
# | title | file size |
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1 | 唐古拉DBY大本营水文观测2009年数据集.xlsx | 10.6 KiB |
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