The strong wind directional shear was maintained by introducing a "nudging' term in the equation of motion to guide the modeled winds in the layers above the ridge top toward the observed wind direction. The second modification was accomplished by reformulating the conservation equation for the potential temperature in such a way that only the deviation from the horizontally averaged value was prognostically computed. The vegetation distribution used in this study is undoubtedly crude. Nevertheless, the present simulation suggests that tall tree canopy can play an important role in producing inhomogeneous wind distribution, particularly in the levels below the canopy top. -from Authors
CITATION STYLE
Yamada, T., & Bunker, S. (1989). A numerical model study of nocturnal drainage flows with strong wind and temperature gradients. Journal of Applied Meteorology, 28(7), 545–554. https://doi.org/10.1175/1520-0450(1989)028<0545:ANMSON>2.0.CO;2
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