'Isentropic surface' diaporamas de présentation

Isentropic Analysis Techniques: Basic Concepts

752 views • 57 slides

40-70 Day Meridional Propagation of Global Circulation Anomalies ( A Global Convection Circulation Paradigm for the Ann

40-70 Day Meridional Propagation of Global Circulation Anomalies ( A Global Convection Circulation Paradigm for the Annular Mode) . Ming Cai 1 and R-C Ren 1,2 1 Department of Meteorology Florida State University, USA 2 LASG, Institute of Atmospheric Physics, CAS, Beijing, P. R. China.

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* Reading Assignments:

* Reading Assignments:. 3.1 3.1.1 3.2 3.3 3.4 3.4.1 3.4.2 3.5 3.6 3.6.1. 4. The Second Law. 4.1 Reversible vs Irreversible processes. Reversible : A process for which a system can be restored to its

467 views • 27 slides

Isentropic Analysis Techniques: Basic Concepts

Isentropic Analysis Techniques: Basic Concepts. March 5, 2004 Adapted from Professor Jim Moore of St. Louis University. Potential temperature as a vertical coordinate.

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CONCEPT OF CONVEYER BELT IN FRONTS AND WAVES

CONCEPT OF CONVEYER BELT IN FRONTS AND WAVES. CONCEPTUAL MODEL. Vertical motion is responsible for layered clouds. Not measured directly. Indirectly measured from Horizontal winds NWP. Normal charts only depict horizontal motion. Clouds patterns reflect relative wind flow.

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February 21, 2006 Lab

February 21, 2006 Lab. Dan Kurz & Matt Chyba Team 4. Analysis Summary Visible Satellite maps

338 views • 19 slides