A model of a stationary planetary boundary layer is proposed based on the equation of motion with the advective term retained. The latter is modeled by means of the so-called geostrophic momentum approximation in two versions -original and modified. New expressions for the vertical velocity W, at th
β¦ LIBER β¦
An Inertial Model of the Interaction of Ekman Layers and Planetary Islands
β Scribed by Pedlosky, Joseph
- Book ID
- 120617773
- Publisher
- American Meteorological Society
- Year
- 2013
- Tongue
- English
- Weight
- 903 KB
- Volume
- 43
- Category
- Article
- ISSN
- 0022-3670
No coin nor oath required. For personal study only.
π SIMILAR VOLUMES
A barotropic model of the Ekman planetar
β
S. Panchev; T. S. Spassova
π
Article
π
1987
π
Springer
π
English
β 411 KB
Ekman boundary layer interactions in a n
β
P. J. Everson; D. R. Davies
π
Article
π
1972
π
John Wiley and Sons
π
English
β 510 KB
## Abstract A representation of an βEkmanβ type of boundary layer (assumed to extend from 1,000 mb to 900 mb) is inserted into a twoβlevel, quasiβgeostrophic, general circulation numerical model. An approximate timeβdependent analytic solution of this boundary layer is matched to the βfree atmosphe
On the interaction of topography and Ekm
β
P. J. Mason; R. I. Sykes
π
Article
π
1978
π
John Wiley and Sons
π
English
β 987 KB
An Analytical Study of the Diurnal Varia
β
Zhe-Min Tan; Majid M. Farahani
π
Article
π
1998
π
Springer
π
English
β 250 KB
Laser-plasma interaction in the context
β
C. Labaune; K. Lewis; H. Bandulet; S. Depierreux; S. HΓΌller; P. E. Masson-Labord
π
Article
π
2007
π
Springer
π
English
β 227 KB
A two-dimensional and steady-state numer
β
Hu Yinqiao; Su Congxian; Ge Zhengmo
π
Article
π
1988
π
Springer-Verlag
π
English
β 608 KB