Abstract

In this model, we investigate compressible and non-hydrostatic wet atmospheric fluid motion for topography, such as a mountainous urban area. We have established basic equations for a generalized coordinate system and have proceeded to the vertical sensitivity test of this model through calculating vertical wind velocity. The distribution pattern and the value of vertical wind velocity are found to be reasonable.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call