topographic amplification factor
A ratio, calculated solely from topographic (terrain elevation) data, of the diurnal
in a valley to that at the same altitude
over the adjacent plain.
The diurnal amplitude is larger (or "amplified") over the valley than over the plain because the volume of air is less in the valley, but the amount of heating or cooling is approximately the same in both locations. The significance of the temperature
differential caused by this amplification is that it produces a horizontal pressure gradient
between the valley and the surrounding plains, or along the axis of the valley itself, that reverses twice per day, driving the diurnally varying along- valley wind system
, upvalley during the day and downvalley at night. See upvalley wind
, downvalley wind
McKee, T. B., and R. D. O'Neal 1989. The role of valley geometry and energy budget in the formation of nocturnal valley winds. J. Appl. Meteor.. 28. 445–456.
Steinacker, R. 1984. Area-height distribution of a valley and its relation to the valley wind. Contrib. Atmos. Phys.. 57. 64–71.
Whiteman, C. D. 1990. Observations of thermally developed wind systems in mountainous terrain. Meteor. Monogr.. No. 45, 9–13.
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