Download presentation
Presentation is loading. Please wait.
1
Thermodynamics Atmosphere
Moisture and atmospheric stability
2
Vertical Structure of the Atmosphere
What is the pressure vertical gradient of the atmosphere?
3
Processes That Lift Air – orographic lifting
4
Processes That Lift Air: frontal lifting
5
Processes That Lift Air: convergence
6
Processes That Lift Air: Localized convective lifting
7
Poisson Equation
8
Adiabatic Temperature Changes
9
Environmental Lapse Rate
10
Environmental Lapse Rate
11
Atmospheric Stability
12
Atmospheric Stability
13
Stability and Daily Weather
Instability is enhanced by: Intense warming of the lowest layer of the atmosphere Heating of an air mass from below Wintertime polar air moves southward over the great lakes Radiation cooling from cloud tops Stability is enhanced by: Radiation cooling of Earth’s surface after sunset Cooling of an air mass from below as it traverses cold surfaces Warm air from the Gulf of Mexico moves northward to the cold land of Midwest in winter
Similar presentations
© 2024 SlidePlayer.com. Inc.
All rights reserved.