Atmosphere and climate 1.1.a GLOBAL ATMOSPHERIC CIRCULATION
- Created by: henryosei2005
- Created on: 05-11-18 16:21
Fullscreen
Global Atmospheric circulation:
Air rises at the equator leading to low pressure and rainfall.
When the air reaches the edge of atmosphere it cannot go any further and so it travels to the north and south.
The air becomes colder and denser…
Comments
No comments have yet been made