
The Diabatic Pressure Difference: A New Diagnostic for the Analysis of Valley Winds
Author(s) -
Juerg Schmidli
Publication year - 2012
Publication title -
monthly weather review
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.862
H-Index - 179
eISSN - 1520-0493
pISSN - 0027-0644
DOI - 10.1175/mwr-d-11-00128.1
Subject(s) - diabatic , forcing (mathematics) , climatology , turbulence , measure (data warehouse) , meteorology , atmospheric sciences , environmental science , geology , physics , computer science , adiabatic process , database , thermodynamics
The purpose of this article is to introduce a new diagnostic measure of the time-integrated diabatic (thermal) forcing of a valley–plain system. This measure can be used to synchronize the evolution of thermally induced valley winds with respect to their forcing. Differences among numerical models or model configurations originating from diabatic forcing versus those originating from the model dynamics (e.g., turbulence scheme, dynamical core, etc.) can then be distinguished.