Slide 14.2 Moist air thermodynamics (Reading Text 3.5-3.7, p79-101) Reading: Trenberth et al. 2005 Climate dynamics, S for water vapor increase with temperature Emanuel 2005,…

Slide 1Cloud Development and Precipitation Prof. John Toohey-Morales, CCM St. Thomas University Miami Gardens, Florida Slide 2 Adiabatic Cooling and Warming Rising air expands…

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Slide 1 THE DISTINCTION BETWEEN LARGE- SCALE AND MESOSCALE CONTRIBUTION TO SEVERE CONVECTION: A CASE STUDY EXAMPLE Paper by Charles A. Doswell III Powerpoint by Christopher…

Slide 1 NATS 101 Lecture 12 Vertical Stability Slide 2 Tennis Basics Racket velocity before hit Ball speed approaching Ball speed leaving Forehand: Racket velocity before…

Thunderstorms Review of last lecture Two types of lightning (cloud-to-cloud 80%, cloud-to-ground 20%) 4 steps of lightning development. How fast does thunder travel? Climate…

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A stable atmosphere. An absolutely stable atmosphere exists when a rising air parcel is colder and heavier (i.e., more dense) than the air surrounding it. If given the chance…

Thermodynamics M. D. Eastin Water Vapor in the Air How do we compute the dewpoint temperature, the relative humidity, or the temperature of a rising air parcel inside a cloud?…