Zentralanstalt für Meteorologie und Geodynamik INITIATION OF AIRMASS DEEP MOIST CONVECTION Thomas Krennert, [email protected],[email protected].
Chapter 7: convective initiation squall line development in Illinois a visible satellite image loop of CI in the eastern US 35°N 103°W Fig. 7.2.
Chapter 09 Cloud Formation Lesson 27-28-29
Overview of Tropical Cyclones AOS 453 April 2004 J. P. Kossin CIMSS/UW-Madison.
INITIATION OF AIRMASS DEEP MOIST CONVECTION
SEVERE WEATHER Lecture 9. Definition of a Severe Thunderstorm The National Weather Service defines a severe thunderstorm as a thunderstorm that produces.
Thunderstorms Conditions required: 1. Conditional instability 2. Trigger Mechanism (eg. front, sea-breeze front, mountains, localized zones of excess surface.
Ice Storms Caused by an accumulation of freezing rain Among the most devastating winter weather events Can halt air and ground transportation Can weigh.
1 Dry Convection Phenomenology, Simulation and Parameterization of Atmospheric Convection Pier Siebesma Yesterday: “Dry” Atmospheric Convection Today:
Mesoscale Gravity Waves
High-resolution Observations and Model Simulations of the Life Cycle of an Intense Mesoscale Snowband over the Northeastern United States Reporter: Prudence.
Investigating Mesoscale Precipitation Banding in Two East Coast Snowstorms