Cumulus Forced; pushed upward by external forces, i.e. lifting by surface convergence, topography etc. Active; growing upward from self-forcing, i.e. buoyancy,
Symmetric instability Sources: Texts: – Martin p. 224-228 – Holton p. 277-281 – Lackmann does not cover this topic Meted modules: – an operational approach.
USE OF HS3 DATA TO UNDERSTAND THE TROPICAL CYCLONE OUTFLOW LAYER John Molinari, Kristen Corbosiero, Stephanie Stevenson, and Patrick Duran University at.
When advection destroys balance, vertical circulations arise COMET-MSC Winter Weather Course 29 Nov. - 10 Dec. 2004 ppt started from one by James T. Moore.
When advection destroys balance, vertical circulations arise
