A New Land Surface Hydrology within the Noah-WRF Land-Atmosphere Mesoscale Model Applied to Semiarid Environment: Evaluation over the Dantiandou Kori (Niger)
Figure 8
As in Figure 7 but for land surface energy budget variables averaged over a 10-day period. All related statistics are given in Table 2. Note that for the latent and sensible heat fluxes, each period were there is not enough day of observation (5 days) to perform an average have been removed.
