A decreasing glacier mass balance gradient from the edge of the Upper Tarim Basin to the Karakoram during 2000–2014

• Published in: Scientific reports 2017-07, Vol.7 (1), p.6712-9, Article 6712
• Main Authors: Lin, Hui, Li, Gang, Cuo, Lan, Hooper, Andrew, Ye, Qinghua
• Format: Article
• Language: English
• Subjects: 704/106/125; 704/106/35/823; Altimetry; Elevation; Glacier mass balance; Glaciers; Humanities and Social Sciences; Interferometry; Mountains; multidisciplinary; Science; Science (multidisciplinary)
• ISSN: 2045-2322; 2045-2322
• DOI: 10.1038/s41598-017-07133-8

In contrast to the glacier mass losses observed at other locations around the world, some glaciers in the High Mountains of Asia appear to have gained mass in recent decades. However, changes in digital elevation models indicate that glaciers in Karakoram and Pamir have gained mass, while recent laser altimetry data indicate mass gain centred on West Kunlun. Here, we obtain results that are essentially consistent with those from altimetry, but with two-dimensional observations and higher resolution. We produced elevation models using radar interferometry applied to bistatic data gathered between 2011 and 2014 and compared them to a model produced from bistatic data collected in 2000. The glaciers in West Kunlun, Eastern Pamir and the northern part of Karakoram experienced a clear mass gain of 0.043 ± 0.078~0.363 ± 0.065 m w.e. yr −1 . The Karakoram showed a near-stable mass balance in its western part (−0.020 ± 0.064 m w.e. yr −1 ), while the Eastern Karakoram showed mass loss (−0.101 ± 0.058 m w.e. yr −1 ). Significant positive glacier mass balances are noted along the edge of the Upper Tarim Basin and indicate a decreasing gradient from northeast to southwest.