Table 3 Glacier mass balance information based on ground observation58 and remote sensing monitoring on the QTP55.
From: Spatiotemporal dynamic characteristics of typical temperate glaciers in China
Glacier name | Mass balance | Ground monitoring | Remote-sensing monitoring | ||||
---|---|---|---|---|---|---|---|
Lon | Lat | Period | Name of glacier area | Mass balance | Period | ||
Palong Glacier No. 4 | − 0.37 ± 0.36 | 96.98 | 29.39 | 1980–2015 | Hindu Raj | − 0.11 ± 0.13 | 1973–2000 |
Hailuogou Glacier | − 0.34 ± 0.44 | 101.92 | 29.58 | 1989–1999 | Spiti Lahaul | − 0.04 ± 0.1 | 1973–2000 |
Demla Glacier | − 1.02 ± 0.55 | 97.02 | 29.36 | 2007–2010 | West Kunlun | 0.02 ± 0.1 | 1973–2000 |
Palon Glacier No. 94 | − 0.90 ± 0.56 | 96.98 | 29.39 | 2006–2016 | Mudu Tag | − 0.06 ± 0.12 | 1975–2000 |
Kangwure Glacier | − 0.51 ± 0.23 | 85.82 | 28.47 | 1992–2010 | West Nepal | − 0.23 ± 0.18 | 1975–2000 |
Namunani Glacier | − 0.42 ± 0.16 | 81.28 | 30.45 | 2006–2010 | Central Nepal | − 0.28 ± 0.11 | 1974–2000 |
Muztag Peak Glacier | − 0.18 ± 0.41 | 75.06 | 38.24 | 2006–2010 | Sikkim | − 0.30 ± 0.12 | 1975–2000 |
Guren River Glacier | − 0.31 ± 0.47 | 90.24 | 30.21 | 2006–2010 | Nyainqentanglha | − 0.25 ± 0.15 | 1975–2000 |
Palong Glacier No. 10 | − 0.78 ± 0.48 | 96.90 | 29.29 | 2006–2009 | Geladandong | − 0.22 ± 0.12 | 1976–2000 |
Palong Glacier No. 12 | − 1.70 ± 0.49 | 96.90 | 29.30 | 2006–2010 | Yigong River | − 0.11 ± 0.14 | 1975–2000 |
Zhuxi Glacier | − 0.52 ± 0.57 | 91.45 | 30.87 | 2008–2010 | Palung River | − 0.19 ± 0.14 | 1974–2000 |
Qiyi Glacier | − 0.18 ± 0.37 | 97.76 | 39.24 | 1975–2010 | |||
Small Dongkemadi Glacier | − 0.27 ± 0.38 | 92.06 | 33.08 | 1989–2010 |