Geostrophic wind flows parallel to isobars when the pressure gradient force and Coriolis force are balanced. This occurs at high altitudes above the friction layer.
Explanation:
Wind gradient is the change in wind speed with altitude. Near the surface, friction reduces wind speed; at higher altitudes, wind speed generally increases.
Explanation:
London is prone to advection fog (also known as sea fog) when warm, moist air from the Atlantic moves over the cooler landmass, cooling to its dew point and forming fog.
Explanation:
Tamil Nadu receives a significant portion of its annual rainfall from the Northeast Monsoon (October-December), making it a crucial season for agriculture there.
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