Abstract:Acoustic sounder measurements of the temperature structure parameter were obtained at the edge of an escarpment which is part of a ridge of mountains. These measurements indicate that in mountainous terrain, the daytime two-dimensional field of thermal turbulence is strongly affected by relative sun-slope orientation and wind direction out to ranges of at least 200-300 m. For the geometry of this site, westerly flow results in a field which tends to decrease rapidly to the west in the morning with a much less … Show more
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