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