Effects of Glacier and Geomorphology on the Mechanism Difference of Glacier-Related Debris Flow on the South and North Banks of Parlung Zangbo River, Southeastern Tibetan Plateau

Table 2

Glaciers along the Parlung river from Bomi to Suotong.

Location	Types of glacier	Number of glaciers and percentage		Area of glaciers (km^2) and percentage		Volume of glaciers (10^6 × m^3) and percentage		Average snow line (m)
North bank	Hanging glacier	18	20.93%	41.12	30.84%	2867.45	33.93	4040
	Cirque glacier	10	11.63%	4.96	3.72%	142.57	1.69%
	Valley glacier	0	0%	0	0%	0	0%
South bank	Hanging glacier	23	26.74%	31.18	23.38%	2058.01	24.35%	3429
	Cirque glacier	15	17.44%	5.82	4.36%	194.73	2.30%
	Valley glacier	20	23.26%	50.27	37.70%	3188.54	37.73%
Sum total	—	86	100%	133.35	100%	8451.3	100%	—