4.2 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.
Cloud Development and Precipitation Prof. John Toohey-Morales, CCM St. Thomas University Miami Gardens, Florida.
Pg class 18 (some 17)
GEU 0047: Meteorology Lecture 6 Stability and Cloud Development.
Simulating Adiabatic Parcel Rise Presentation by Anna Merrifield, Sarah Shackleton and Jeff Sussman.
THE DISTINCTION BETWEEN LARGE- SCALE AND MESOSCALE CONTRIBUTION TO SEVERE CONVECTION: A CASE STUDY EXAMPLE Paper by Charles A. Doswell III Powerpoint by.
NATS 101 Lecture 12 Vertical Stability. Tennis Basics Racket velocity before hit Ball speed approaching Ball speed leaving Forehand: Racket velocity before.
Thunderstorms. Review of last lecture 1.Two types of lightning (cloud-to-cloud 80%, cloud-to- ground 20%) 2.4 steps of lightning development. 3.How fast.
Thunderstorms and Lightning. Review of last lecture Bergeron process: happens with coexistence of ice and super- cooled water. Key: Saturation vapor pressure.
youtube/watch?v=2mTLO2F_ERY
Chapter 5: Cloud Development and Precipitation Atmospheric Stability Atmospheric Stability Determining stability Determining stability Cloud development.
ThermodynamicsM. D. Eastin Water Vapor in the Air How do we compute the dewpoint temperature, the relative humidity, or the temperature of a rising air.