Research Article

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

Table 1

Simulated surface atmospheric variables versus in situ measurements in Wankama: Precipitation, P (mm/day); Relative humidity, Rh (%); 2 m air temperature, Ta (K); downward Shortwave, SW, and Longwave, LW, radiations (W/m²); Wind speed, Ws (m/s). The Mean, standard deviation ( ), Bias, RMSE, correlation (r), and efficiency (Eff) are given for all variables at a 3-hour time step, excepted for precipitation (daily).

VariablesObs ExpMeanσBiasRMSErEff

P1.736.92CTL2.3715.700.6416.60.08
PHY1.9611.940.2312.60.18
Rh38.7428.06CTL30.6822.39 13.60.930.77
PHY35.3925.83 10.30.940.86
Ta302.335.23CTL304.274.901.943.20.880.64
PHY303.494.931.162.80.880.71
SW245.14327.25CTL270.25370.2425.10149.70.920.79
PHY272.73371.1427.58143.70.930.81
LW382.3240.49CTL399.6439.7517.3225.60.890.60
PHY398.3338.6416.0224.40.890.64
Ws3.081.71CTL3.531.440.452.00.26
PHY3.461.420.391.90.29