Thunderstorms - Introduction
- Are many types
- usually form in an unstable
environment - in the mT air mass
- often triggered by:
- strong surface heating
- terrain
- frontal boundaries -
examples:
- cold, warm fronts
- sea-breeze fronts
- dryline
- act to transport warm, moist air
aloft, and bring down cool air to the surface
- hence, thunderstorms act to stablize the atmosphere
|
image adopted
from Meteorology Today by C. Donald Ahrens © 1994
West Publishing Company |