| 1. |
- ANDREN, A
(författare)
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THE STRUCTURE OF STABLY STRATIFIED ATMOSPHERIC BOUNDARY-LAYERS - A LARGE-EDDY SIMULATION STUDY
- 1995
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Ingår i: QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY. - : ROYAL METEOROLOGICAL SOC. - 0035-9009. ; 121:525, s. 961-985
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Tidskriftsartikel (refereegranskat)abstract
- Dry stably-stratified planetary boundary layers have been studied by large-eddy simulation. Results from simulations using two different subgrid-scale models are compared. A recently suggested improved subgrid-scale model version is shown to give improve
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| 2. |
- Enger, L, et al.
(författare)
-
The response of bora-type flow to sea surface temperature
- 1998
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Ingår i: QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY. - : ROYAL METEOROLOGICAL SOC. - 0035-9009. ; 124:548, s. 1227-1244
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Tidskriftsartikel (refereegranskat)abstract
- A non-linear, two-dimensional, hydrostatic, incompressible numerical model with a higher-order turbulence closure scheme is used to study the effect of sea surface temperature on the severe downslope wind called bora at the Adriatic coast. A non-linear la
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| 3. |
- GRISOGONO, B
(författare)
-
A GENERALIZED EKMAN LAYER PROFILE WITH GRADUALLY VARYING EDDY DIFFUSIVITIES
- 1995
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Ingår i: QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY. - : ROYAL METEOROLOGICAL SOC. - 0035-9009. ; 121:522, s. 445-453
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Tidskriftsartikel (refereegranskat)abstract
- The classical analytical solution for the Ekman layer flow has been generalized by introducing an assigned non-rapidly-varying eddy diffusivity K(z). Asymptotic expressions for the wind components u, nu Q obtained via the WKB method retain the form and,
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