We present a study of the impact of the flooding of two depressions, which are not flooded yet, on the regional environment and weather. For this purpose, we used the WRF-NOAHMP model in combination with a dynamic lake model (WRF-NOAHMP-LAKE). The model was forced by ERA5 data during June 2017 and operated either without (Control) and with (Impact) of the flooding effect.
Over and in the region of the artificial lakes, we found substantial effects on the surface water and land surface temperature fields as well as the atmospheric 2-m surface temperature and moisture fields. Also the depth of the planetary boundary layer was reduced. In the impact runs, the diurnal cycle of the 2-m temperature was damped by up to 4 degrees in comparison to the control and the surface moisture was enhanced by 3 g/kg. Particularly interesting was a change of the sea breeze and related convergence zones in the region of the artificial lake, which - in combination with a modification of the PBL structure - resulted in an enhancement of cloudiness and even of precipitation southwesterly of the lake and over the southern part of the lake.
Overall, a substantial positive impact on the regional environment and the weather pattern was found. Therefore, it is worthwhile to consider a realization of this flooding project to support economic and agricultural projects in a continental desert region.