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above the freezing point of water, the ice crystal will melt and fall as rain. However, if the melting raindrop passes through a freezing layer, it will refreeze and reach the ground as ice pellets, or frozen raindrops. Finally, if the ice crystal melts, only to reenter freezing air just at ground level, it will strike the ground as freezing rain. If the water vapor comes in direct contact with the cooler surface, it can condense onto it. Fog can occur when warm air moves into an area that has a cold surface temperature. An advected fog forms in this situation. This also can be a reverse situation, where cooler air moves over a warmer surface. Ground fog forms by radiational cooling at night. These are common in humid valleys and near rivers and lakes. Where the air pressure at the surface is low, air rises and The hottest product book lovers reading books fall open you fall in tote bagbecomes cooler. The water vapour in it begins to condense into tiny drops of water or, if it is cold enough, into tiny ice crystals. If there is enough water or ice, rain or snow begins to fall. This is why areas of low pressure are associated with bad weather. Anticyclones form when air currents in the high and middle atmosphere converge, piling up air in one area. The air inside these areas sinks from high levels towards the earth’s surface. The sinking air is warmed by compression, and this evaporates any cloud. This is why high pressure is

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