FratFiles

• Save Paper

The global energy balance and atmospheric motion mainly determine

the circulation of the earth's atmosphere. There is a hierarchy of motion

in atmospheric circulation. Each control can be broken down into smaller

controlling factors. The global energy balance is an equal balance of

short-wave radiation coming into the atmosphere and long-wave radiation

going out of the atmosphere. This is called thermal equilibrium. The

earth is at thermal equilibrium; however, there can have a surplus or

deficit of energy in parts of the heat budget. If you have a net

radiation surplus warm air will rise, and a net radiation deficit will

make the air cool an fall. Air gets heated at the equator because of the

inter tropical convergence zone and rises to the poles. There the air is

cooled and it floats back down to the equator where the process is

repeated. Another major contributing factor to the circulation of the air

is due to the......

View the rest of this paper...

Approximate Word Count: 803
Approximate Pages: 4 (250 words per double-spaced page)

Similar Essays

1. Atmospheric Circulation And More
   

   Atmospheric Circulation And More The global energy balance and atmospheric motion mainly determine the circulation of the earth's atmosphere. There is a hierarchy of motion in

2. Research Paper In Tech Wri
   

   is created, leading to further infrared-radiation absorption. As temperatures increase, atmospheric circulation patterns are altered which will change local weather patterns.

3. Heat Budget
   

   Insolation - The primary source of energy to drive our global climate system (including atmospheric and, to a lesser extent, oceanic circulation) is the heat we receive from the

4. The Atmospheric Ozone Layer
   

   long lifetimes in the troposphere, eventually arrive in the stratosphere through normal atmospheric circulation patterns and may interfere with or destroy the natural ozone

5. Dramatic Fluctuations Of Devil's Lake, Nd
   

   would suspect that the winter/spring precipitation and summer/fall temperature (and hence atmospheric circulation patterns), are most important for diagnosing the changes in the