The Models for the Local and Regional Scales Atmospheric Flows

Abstract

In this chapter, two privileged meteorological situations will be considered as a function of the hydrostatic parameter ε = H/L:

$$\varepsilon \sim {10^{ - 1}} \Rightarrow {\rm{Ro}} \sim {\rm{1;}}$$

(13.1)

and

$$\varepsilon \sim 1 \Rightarrow {\rm{Ro}} \gg {\rm{1}}\,\,{\rm{.}}$$

(13.2)