Eddies of small diameters (a few meters or less), disperse smoke, sway branches & swirl dust & papers into the air, are usually short-lived (last only a few minutes at best)
Mesoscale
Range from a few kilometers to about a hundred kilometers in diameter, last longer (often many minutes, hours, or in some cases as long as a day), include local winds along shorelines and mountains, thunderstorms, tornadoes, & small tropical storms
Macroscale
Synoptic scale: dominate regions of hundreds to even thousands of square kilometers, typically last for days & sometimes weeks
Macroscale
Planetary (Global) scale: largest wind patterns ranging over the entire earth
General Atmospheric Circulation
The average flow of air in the entire globe, based on wind observations (20 or more years), complex pattern of winds & pressure systems, the underlying cause is the unequal heating of the earth's surface
Single-Cell Model
Assumptions: The earth's surface is uniformly covered with water, differential heating between land and water does not come into play, The sun is always directly over the equator, winds will not shift seasonally, The earth does not rotate, only pressure gradient force is present
Three-Cell Model
The tropical regions still receive an excess energy and the poles a deficit, In each hemisphere, 3 cells instead of 1 take the task of energy redistribution
Features of Three-Cell Model
Polar Cell
Ferrel Cell
Hadley Cell
Features of Three-Cell Model with land and water distribution