Warning: Use of undefined constant referer - assumed 'referer' (this will throw an Error in a future version of PHP) in /usr/home/essaywo/public_html/essays on line 102

Warning: Use of undefined constant host - assumed 'host' (this will throw an Error in a future version of PHP) in /usr/home/essaywo/public_html/essays on line 105

Warning: Cannot modify header information - headers already sent by (output started at /usr/home/essaywo/public_html/essays:102) in /usr/home/essaywo/public_html/essays on line 106

Warning: Cannot modify header information - headers already sent by (output started at /usr/home/essaywo/public_html/essays:102) in /usr/home/essaywo/public_html/essays on line 109
Atmospheric Circulation And More - Term Papers

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 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 ...

Want to read the rest of this paper?
Join Essayworld today to view this entire essay
and over 50,000 other term papers

winds and

calms ranges from 5 degrees north to 5 degrees south. This wind belt is

characterized by weak winds and low pressure from the inter tropical

convergence zone. As you go further north or south you encounter the

Hadley Cells. Hadley cell circulation is caused by the movement of high

pressure from the latitudes at 5 to 30 degrees north and 5 to 30 degrees

south to low pressure areas around the equator.

The movement of air from high pressure to low pressure causes

convergence. This convergence generates the production of wind. The

winds that are produced from this are the trade winds. The winds blow

from a northwest direction in the northern hemisphere, and in the southern

hemisphere the winds blow from a southeast direction. The trade winds are

the largest wind belt. The westerlies, they lie between 35 and 60 degrees

north and south latitude. The wind blows from the west , thus their name.

The westerlies are in the ...

Get instant access to over 50,000 essays.
Write better papers. Get better grades.

Already a member? Login

CITE THIS PAGE:

APA
MLA
Chicago
Turabian

Atmospheric Circulation And More. (2006, December 14). Retrieved November 28, 2024, from http://www.essayworld.com/essays/Atmospheric-Circulation-And-More/57084

"Atmospheric Circulation And More." Essayworld.com. Essayworld.com, 14 Dec. 2006. Web. 28 Nov. 2024. <http://www.essayworld.com/essays/Atmospheric-Circulation-And-More/57084>

"Atmospheric Circulation And More." Essayworld.com. December 14, 2006. Accessed November 28, 2024. http://www.essayworld.com/essays/Atmospheric-Circulation-And-More/57084.

JOIN NOW

Join today and get instant access to this and 50,000+ other essays

PAPER DETAILS

Added: 12/14/2006 03:17:08 AM
Category: Science & Nature
Type: Free Paper
Words: 685
Pages: 3

Save |

Report

SHARE THIS PAPER

SAVED ESSAYS

Save and find your favorite essays easier