Coupling Analysis of Hydrometeorology and Erosive Landforms Evolution in Loess Plateau, China

Table 1

Parameters configuration of Erosive Landform Evolution Index (ELEI).

Parameters of Erosive Landform Evolution Index	Weihe River	Jinghe River	Beiluo River	Wudinghe River
Gully
Gully density (km/km^2)	0.13	0.15	0.15	0.13
Runoff (10^8 m^3)	64.62	16.01	8.16	10.86
Sediment discharge (10^8 t)	2.94	2.08	0.68	0.92
RDLS
0–20	0.44%	0.23%	0.61%	1.67%
20–75	5.81%	1.01%	3.96%	37.30%
75–300	29.82%	52.36%	58.94%	53.12%
300–600	42.31%	44.49%	36.45%	7.85%
600–max	21.62%	1.91%	0.04%	0.06%
Runoff (10^8 m^3)	64.62	16.01	8.16	10.86
Sediment discharge (10^8 t)	2.942	2.083	0.682	0.916
Slope (°)
0~5	24.32%	16.69%	19.12%	57.46%
6~15	38.14%	40.77%	41.05%	27.89%
16~25	23.98%	32.75%	29.54%	11.94%
26~35	9.56%	6.24%	8.85%	2.31%
36~40	2.20%	2.92%	0.88%	0.22%
41~45	1.08%	0.30%	0.31%	0.09%
46~max	0.73%	0.34%	0.24%	0.09%
Runoff (10^8 m^3)	64.62	8.16	16.01	10.86
Sediment discharge (10^8 t)	2.942	0.682	2.083	0.916
ELEI
Gully length (km)	9334.05	3501	5865.51	4414.58
RDLS (km^2, 20–600 m)	48825.22	26755.75	44496.04	29713.77
Slope (km^2, 0–25°)	54150.01	24294.27	40790.31	29417.45