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Parametrization of orographical effects in the planetary boundary layer

โœ Scribed by D. Yordanov; N. Godev


Publisher
Springer
Year
1973
Tongue
English
Weight
586 KB
Volume
5
Category
Article
ISSN
0006-8314

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โœฆ Synopsis


Studies of the influence of orography on the dynamics of atmospheric processes usually assume the following relation as a boundary condition at the surface of the Earth, or at the top of the planetary layer:

where u, v and w are the components of wind velocity along the x, y and z axes, respectively, and z0 = zo(x, y) is the equation of the Earth's orography. We see that w, and consequently the influence of orography on the dynamics of atmospheric processes, depend on the wind (u, v) and on the slope of the obstacle (zo/Jx, 6zo/y).

In the present work, it is shown that the above relation for w is insufficient to describe the influence of orography on the dynamics of the atmosphere. It is also shown that the relation is a particular case of the expression:

Wh

a,=lv, [(Ros) O + a2(Ro, s) &yj + wh VgI [ai RoszoX +I Ivg1 2 r 6 2 zo 62zO 62zo b (Ro, s + b (Ro, s) Vx + 2 1o, b a s (Ro,


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