+ All Categories
Home > Documents > General Circulation of the Atmosphere. Hadley Cell.

General Circulation of the Atmosphere. Hadley Cell.

Date post: 15-Jan-2016
Category:
View: 215 times
Download: 0 times
Share this document with a friend
Popular Tags:
36
General Circulation of the Atmosphere
Transcript
Page 1: General Circulation of the Atmosphere. Hadley Cell.

General Circulation of the Atmosphere

Page 2: General Circulation of the Atmosphere. Hadley Cell.

Hadley Cell

Page 3: General Circulation of the Atmosphere. Hadley Cell.
Page 4: General Circulation of the Atmosphere. Hadley Cell.
Page 5: General Circulation of the Atmosphere. Hadley Cell.
Page 6: General Circulation of the Atmosphere. Hadley Cell.
Page 7: General Circulation of the Atmosphere. Hadley Cell.

Monsoons

A monsoon is a term from early Arabs called the "Mausin," or "the season of winds." This was in reference to the seasonally shifting winds in the Indian Ocean and surrounding regions, including the Arabian Sea.

Page 8: General Circulation of the Atmosphere. Hadley Cell.

Indian Monsoon

SW US Monsoon

Page 9: General Circulation of the Atmosphere. Hadley Cell.

Monsoon

Page 10: General Circulation of the Atmosphere. Hadley Cell.
Page 11: General Circulation of the Atmosphere. Hadley Cell.

Monsoon Origin

Page 12: General Circulation of the Atmosphere. Hadley Cell.

West African Monsoon

Page 13: General Circulation of the Atmosphere. Hadley Cell.
Page 14: General Circulation of the Atmosphere. Hadley Cell.

Southwest U.S. Monsoon

Page 15: General Circulation of the Atmosphere. Hadley Cell.
Page 16: General Circulation of the Atmosphere. Hadley Cell.
Page 17: General Circulation of the Atmosphere. Hadley Cell.
Page 18: General Circulation of the Atmosphere. Hadley Cell.

The Jet Stream

• A long, narrow current of strong winds in the midlatitudes that is generally found in the upper troposphere and lower stratosphere (roughly 25,000-35,000 ft, 400-250 hPa).

• First became obvious during WWII as high flying aircraft was sped up and slowed down on their missions.

• Strongest can exceed 200 mph. Nearly always from the west in midlatitudes

Page 19: General Circulation of the Atmosphere. Hadley Cell.

B-29s flying westward to Japan

Page 20: General Circulation of the Atmosphere. Hadley Cell.

Jet Streams are NOT uniform

Page 21: General Circulation of the Atmosphere. Hadley Cell.
Page 22: General Circulation of the Atmosphere. Hadley Cell.

Jet Streams Associated with Horizontal Temperature Gradients

Page 23: General Circulation of the Atmosphere. Hadley Cell.

Air Masses

Page 24: General Circulation of the Atmosphere. Hadley Cell.
Page 25: General Circulation of the Atmosphere. Hadley Cell.
Page 26: General Circulation of the Atmosphere. Hadley Cell.

Maritime Tropical Source Region

Page 27: General Circulation of the Atmosphere. Hadley Cell.

Continental Polar Source Region

Page 28: General Circulation of the Atmosphere. Hadley Cell.

Continental Tropical Source Region

Page 29: General Circulation of the Atmosphere. Hadley Cell.
Page 30: General Circulation of the Atmosphere. Hadley Cell.

Maritime Polar

Page 31: General Circulation of the Atmosphere. Hadley Cell.

Bering Sea Cloud Streets

Page 32: General Circulation of the Atmosphere. Hadley Cell.
Page 33: General Circulation of the Atmosphere. Hadley Cell.
Page 34: General Circulation of the Atmosphere. Hadley Cell.
Page 35: General Circulation of the Atmosphere. Hadley Cell.
Page 36: General Circulation of the Atmosphere. Hadley Cell.

Recommended