Severe convective storms, theory Pieter Groenemeijer FMI Helsinki, 2 May 2005.
Atmospheric Destabilization Processes Upper Level Mixed Layer Synoptic Lifting Dynamic Destabilization Differential Advection.
Lapse Rates & Stability Learning outcomes: - What are condensation nuclei? - What is the difference between DALR & SALR? - What are the different states.
THE FEDERAL UNIVERSITY OF TECHNOLOGY, AKURE DEPARTMENT OF METEOROLOGY MET 302 ATMOSPHERIC DYNAMICS (Lecture notes prepared by Mr. N. O. Nnoli using some.
Investigating Mesoscale Precipitation Banding in Two East Coast Snowstorms Adam Frumkin.
The Inland Extent of Lake Effect Snow (LES) Bands Joseph P. Villani NOAA/NWS Albany, NY Michael L. Jurewicz, Sr. NOAA/NWS Binghamton, NY Jason Krekeler.
Lecture 23: Map discussion + Thunder & Tornadoes (Ch 11) brief map discussion and/or storm video cloud buoyancy & order-of-magnitude estimate for vertical.
Tropical Cyclones and Hurricanes Read Chapter 11.
Tropical Cyclones and Hurricanes Read Chapter 11
Matilde Nicolini, Yanina García Skabar and Paola Salio CIMA-DCAO-CONICET-UBA- SMN
INITIATION OF AIRMASS DEEP MOIST CONVECTION
II. Synoptic Atmospheric Destabilization Processes Elevated Mixed Layer (EML) Synoptic Lifting Dynamic Destabilization Differential Advection.