THERMAL SOARING FORECASTING Richard Kellerman [email protected] .
Process Lapse Rates When air rises it is depressurized and expands. As a result its temperature falls. When unsaturated air rises, its rate of cooling.
Atmospheric Thermodynamics – III Adiabatic Processes Leila M. V. Carvalho Dept. Geography, UCSB.
1 Buoyancy driven turbulence in the atmosphere Stephan de Roode (TU Delft) Applied Physics Department Clouds, Climate and Air Quality [email protected].
Lecture 13: Map discussion + Cloud development and forms (Ch 6) Quiz 2 next Friday 13 Oct covers to end of Ch. 6 map discussion (situation of Thurs 5 Oct)
ATS 351 ATS 351 Lecture 6 Stability & Skew-T Diagrams.
Quasi-geostrophic theory (Continued) John R. Gyakum.
AOSS 321, Winter 2009 Earth Systems Dynamics Lecture 13 2/19/2009 Christiane Jablonowski Eric Hetland [email protected]@umich.edu [email protected]@umich.edu.
AOSC 200 Lesson 18. Fig. 11-1, p. 312 Lifted Index A parcel of air will not rise unless it is unstable. The lifted index follows a parcel of air as it.
Chapter 6 Introduction to Atmospheric Moisture Physical Geography A Landscape Appreciation, 9/e Animation Edition Victoria Alapo, Instructor Geog 1150.
SEVERE WEATHER Lecture 9. Definition of a Severe Thunderstorm The National Weather Service defines a severe thunderstorm as a thunderstorm that produces.
Introduction to Numerical Weather Prediction 4 September 2012.