Respuesta :
The majority of surface storms and precipitation occur over terrain downstream of troughs (following the horizontal wind direction from a trough to a ridge). In this pattern, a very powerful ridge is located over the state of Alaska, a deep trough is located over Arizona in the western United States.
More than 200 inches of precipitation fall annually on coastal mountain ranges in the southeast Panhandle, compared to 60 inches south of the Alaska Range, 12 inches in the Interior, and less than 6 inches on the North Slope.
Smaller-scale weather phenomena, such as the migration of surface low pressure zones, the motion of hurricanes, and the motion of individual thunderstorm cells, can be significantly influenced by the 500 mb winds. Because it is located in the centre of the atmosphere, meteorologists consider this characteristic to be crucial. The height at which the pressure is 500 mb is known as the 500 mb height. There is low pressure at the surface when the 500mb height is low, and high pressure there when the 500mb height is high.
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