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)
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
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
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
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