:The geostrophic equilibrium is a quasi-equilibrium between the pressure gradient force ( PGF ) and the coriolis force ( CF ).
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A convective downdraft is linked to three forces in the vertical, namely perturbation pressure gradient force, buoyancy force and precipitation loading.
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The pressure gradient force is represented by blue arrows, the Coriolis acceleration ( always perpendicular to the velocity ) by red arrows
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The first term on the right hand side of the above equation represents electromagnetic forces and the second term represents pressure gradient forces.
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Pressure Gradient Force : " The pressure-gradient force is the force which results when there is a difference in pressure across a surface.
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The "'Ekman layer "'is the layer in a fluid where there is a force balance between pressure gradient force, Coriolis force and turbulent drag.
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Beyond the tropics, the dominant forces act in the horizontal direction, and the primary struggle is between the Coriolis force and the pressure gradient force.
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Note that the pressure gradient force points from high towards low pressure zones, it is thus oriented in the opposite direction from the pressure gradient itself.
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As a result, the pressure gradient force has a greater effect and the air still moves from high pressure to low pressure, though with great deflection.
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Movement is driven by the pressure gradient force ( horizontal differences in atmospheric pressure ) and the Coriolis force ( caused by the Earth's rotation on its axis ).
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