A New Land Surface Hydrology within the Noah-WRF Land-Atmosphere Mesoscale Model Applied to Semiarid Environment: Evaluation over the Dantiandou Kori (Niger)

Table 2

As in Table 1 but for the surface energy budget variables: surface net radiation, Rn (W/m²); ground heat flux, G (W/m²); latent heat flux, LE (W/m²); sensible heat flux, H (W/m²).

Variables	Obs	𝜎𝑜𝑏𝑠	Exp	Mean	𝜎	Bias	RMSE	r	Eff
Rn	70.12	182.38	CTL	116.87	233.48	46.75	98.6	0.94	0.71
			PHY	126.96	231.88	56.84	101.2	0.95	0.69
H	33.98	60.98	CTL	96.42	136.97	62.44	108.8	0.87	−2.18
			PHY	92.40	136.24	58.42	106.4	0.86	−2.05
LE	56.35	79.17	CTL	36.50	51.34	−19.85	55.7	0.75	0.51
			PHY	50.44	74.26	−5.91	54.6	0.76	0.52
G	2.88	54.50	CTL	−0.41	78.62	−3.29	48.2	0.80	0.22
			PHY	−0.40	72.55	−3.28	47.1	0.76	0.25