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Tropical Meteorology - uni-muenchen.deroger/...3 ¾Introduction to the tropics ¾The zonal mean circulation (Hadley circulation) ¾The data network in the tropics (field experiments)
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Boundary Layer Meteorology Chapter 11 - uni-muenchen.deroger/Lectures/... · 2003. 6. 23. · Boundary Layer Meteorology Chapter 11 Convective mixed layer ¾The mixed layer is so
LECTURES ON TROPICAL CYCLONES - uni-muenchen.deroger/Lectures/Tropical... · The middle panel shows temperature (upper curve) and dewpoint. When TD >T, both are set to 1 2 (T +TD)
LECTURES ON DYNAMICAL METEOROLOGY - uni-muenchen.deroger/Lectures/Dm_Lectures/... · CHAPTER 1. INTRODUCTION 8 Figure 1.1: Location of upper air stations where measurements of temperature,
Lectures on Tropical Cyclones - uni-muenchen.deroger/Lectures/Tropical...Lectures on Tropical Cyclones Outline of course ¾Introduction, Observed Structure ¾Dynamics of Mature Tropical
Teil I WS2005-09 - meteo.physik.uni-muenchen.deroger/Lectures/Einfuehrung... · Graphische Darstellung von Zustandsänderungen ¾Der thermodynamische Zustand eines Gases läßt sich
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Chapter 3 TROPICAL CYCLONE MOTION - uni-muenchen.deroger/... · TROPICAL CYCLONE MOTION The prediction of tropical cyclone motion has improved dramatically during the last decade
Moist Convection - uni-muenchen.deroger/Lectures/... · 2002. 6. 24. · Moist convection ¾Let us consider the differences between moist convection and dry convection. ¾In dry convection,
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Roger K. Smith - meteo.physik.uni-muenchen.de · Einf uhrung Regnet es morgen? Wie wird das W etter am oc henende? Meteorologie-studen ten w erden solc he F ragen b eliebig oft gestellt
Equations and scaling at low latitudes - uni-muenchen.deroger/Lectures/Tropical... · 1 Equations and scaling at low latitudes The governing equations on a sphere p D1 1 p Dt D Dt
1.2 Vorticity-streamfunction method - uni-muenchen.deroger/Lectures/Tropical... · 1.2 Vorticity-streamfunction method The vorticity-streamfunction method is a powerful way of solving
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Teil I WS2001-01 - meteo.physik.uni-muenchen.deroger/Lectures/Einfuehrung... · Wetterphänome ¾Planetare Wellen ¾Tief- und Hochdruckgebiete der mitteleren Breiten ¾Kalt- und Warmfronten
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Lectures on Tropical Cyclones - uni-muenchen.deroger/Lectures/Tropical... · tropical cyclones, Rev. Geophys. Space Phys., 12, 495-522 ... NOAA WD-P3. Radar display from the tail
Tropical cyclone spin-up revisited - uni-muenchen.deroger/Publications/M3.… · cyclone amplification in a three-dimensional model. In the first paper (Nguyen et al., 2008; henceforth
Die globale Energiebilanz - Teil I - uni-muenchen.deroger/... · Größenordnung von 0,02 W m−2 entspricht. ¾Bei weiterem Ausbau der Kernenergie könnte der Wert bis in hundert
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Boundary Layer Meteorology - uni-muenchen.deroger/Lectures/... · 2006-06-08 · ¾J. R. Garratt The atmospheric boundary layer Cambridge University Press, 1992 ¾R. B. Stull An introduction
Balanced Dyyynamical Theor y - uni-muenchen.deroger/Lectures/Tropical... · Balanced Dyyynamical Theor y The primary and secondary circulations Chapter 3Chapter 3. Inviscid equations
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