Slope and valley wind systems are local thermally driven circulations that form frequently in complex terrain areas. Recent research has focused on the temperature structure along the slope and valley axes that leads to the wind systems. Two new tools being used in...
CITATION STYLE
Whiteman, C. D. (1990). Observations of Thermally Developed Wind Systems in Mountainous Terrain. In Atmospheric Processes over Complex Terrain (pp. 5–42). American Meteorological Society. https://doi.org/10.1007/978-1-935704-25-6_2
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