SUBJECT
Dynamic modelling 2
lecture
master
2+1
Semester 3
Autumn semester
Necessity for simplification of the system of hydro-thermodynamic equations, similarity theory, method of order analysis, quasi-static (primitive) system of equations, approximations to the system of prognosis equations, linearization of the system of atmospheric equations, the five basic modes of atmospheric motions, parameterizations of atmospheric microphysical processes and surface-atmosphere interactions.
George J. Haltiner, 1980, Numerical Prediction and Dynamic Meteorology, John Wiley & Sons, 477 p.