Atmospheric Dynamics | Part 1
The atmosphere is a dynamic system. Temperature changes and the Earth's motion are responsible for horizontal and vertical air displacement. Here the air of the atmosphere circulates between the poles and the Equator in horizontal bands within different latitudes. Moreover, the characteristics of the Earth's surface alter the path of the moving air, causing zones of different air densities. The relations that arise among these processes influence the climatic conditions of our planet.
latitude = a geographic coordinate (line) with the position north or south of the equator measured from 0° to 90°
descend = go down
apparent deflection = the turn aside from a straight course that seems real
deflect = cause something to change direction
rotational velocity = the rotation rate of an object, measured in radians per second