Analysis of microwave precipitation in the topographic barrier for the lifting condensation level of clouds formation

摘要

This paper introduces a physics-based of cloud dynamics that has been considered to calculate the dynamics of rising air parcels in vertically altitude. It is a novel technique to force the lifting condensation level (LCL) by using microwave heating disturbance method to increase the temperature of moist air. The natural process of cloud formation is depended on LCL, relative humidity (R.H.), temperature at altitude (T_d), and surface temperature (T₀). Theoretical analysis investigations were carried out using a microwave heating to increase temperature at surface level for moist air parcels are uplifted vertically at the condensation level. The calculation of liquid water per cubic meter were performed by using commercial software. The initial condition of terrain barrier equal to 2 km. Considering a moist air parcel as energy absorption load and calculate by using different power are equal to 100, 200, 300, 400 and 500 kW, respectively. In this context, the results are compared by considering at the liquid water density values. The advantage of the LCL algorithm and temperature results at various times of microwave heating is that it can be applied to modify the equilibrium of condensation level for the warm orographic cloud formation.