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 1

Typical debris flows along the Parlung River from Bomi to Suotong (e.g. 1–13 in Figure 1).

No.	Name	Date	Size class	Data source	Location
1	Bitong gully	5 Sep. 2007	Middle	Interviews with local residents	North bank
		5 Sep. 2016	Large	Field investigation
2	Dada gully	4 Aug. 2013	Small	Interviews with local residents
		20 Jul. 2017	Middle	Field investigation
3	Jiaolong gully	Sep. 1988	Middle	[14]
		15 Aug. 1989	Large	[14]
		5 Sep. 2016	Middle	Field investigation
4	Cangguo gully	1975	Large	[14]
		1996	Large	[14]
5	Zhataduo gully	Jul. 1987	Large	[14]
6	Naha gully	1968	Super-large	Interviews with local residents
		1978	Large	[14]
		Sep. 2018	Middle	Field investigation
7	Guxiang gully	29 Sep. 1953	Super-large	[28]
		1954	Large	[14]
		1963	Large	[14]
		30 Jul. 2005	Large	Interviews with local residents
		Jul. 2020	Large	Field investigation
8	Suotong gully	26 Jul. 1991	Middle	[14]
9	Qiuzhu gully	2014	Middle	Interviews with local residents	South bank
		28 Aug. 2016	Middle	Field investigation
10	Chidan gully	5 Sep. 2016	Middle	Field investigation
11	Songrao gully	4 Sep. 2007	Large	[32]
		25 Jul. 2010	Large	[32]
		11 Jul. 2018	Large	Field investigation
12	Michong gully	Aug. 2015	Small	Interviews with local residents
13	Danka gully	Aug. 2015	Small	Interviews with local residents