A)- pressure gradient force has its direction always from high pressure zone to low pressure zone, here in this diagram A direction represents pressure gradient force,
B)- in Southern Hemisphere, the direction of the Coriolis force would be leftward with respect to the facial direction, and direction of the friction is always opposite to the direction of the motion air, so here
pressure gradient force - A(discussed earlier)
coriolis force- E
friction force- D( against the direction of motion )
C)- in Northern Hemisphere, the direction of the Coriolis force would be rightward with respect to the facial direction, and direction of the friction is always opposite to the direction of the motion air but when air blows at low height but when it flows at higher altitude their will be no friction force, so here-
A)- pressure gradient force- A
B)- Coriolis force- when air blows along A, then Coriolis force are in direction F; when air blows in direction of F, the Coriolis force would be in direction of D, to neutralise the pressure gradient force A.
992 mb 996 mb F 1000 mb 1004 mb 1. There are three main variables that...
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Name- Date Chapter 6 Laboratory Exercises 1. Consider the Coriolis force in the Southern Hemisphere and its effect on wind direction Following arguments similar to those given in the text (and in Figure 6.25) for the Northerm Hemisphere., (a) explain why the deflection resulting from the Coriolis force in the Southern Hemisphere is to the left. (b) Draw an area of low pressure with a few closed isobars. Label the isobars with realistic values of sea-level pressure....