| 1. |
- Barthelmie, RJ, et al.
(författare)
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Observations and simulations of diurnal cycles of near-surface wind speeds over land and sea
- 1996
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Ingår i: JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES. - : AMER GEOPHYSICAL UNION. - 0148-0227. ; 101:D16, s. 21327-21337
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Tidskriftsartikel (refereegranskat)abstract
- The role of stability and roughness changes in producing diurnal cycles of wind speed offshore is examined using experimental data and numerical simulations. Overnight, the transition from stable conditions over land to less stable conditions over sea com
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| 2. |
- Berger, BW, et al.
(författare)
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The baroclinic, variable eddy viscosity Ekman layer - An approximate analytical solution
- 1998
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Ingår i: BOUNDARY-LAYER METEOROLOGY. - : KLUWER ACADEMIC PUBL. - 0006-8314. ; 87:3, s. 363-380
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Tidskriftsartikel (refereegranskat)abstract
- The WKB method is used in conjunction with the variation of parameters technique to find an approximate analytical solution for Ekman layers with eddy viscosity and horizontal pressure gradient that are each variable with height from the surface. Behavio
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| 3. |
- Cui, ZQ, et al.
(författare)
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Idealized simulations of atmospheric coastal flow along the central coast of California
- 1998
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Ingår i: JOURNAL OF APPLIED METEOROLOGY. - : AMER METEOROLOGICAL SOC. - 0894-8763. ; 37:10, s. 1332-1363
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Tidskriftsartikel (refereegranskat)abstract
- A fully nonlinear, primitive equation hydrostatic numerical model is utilized to study coastal how along central California. combining a realistic atmospheric model, with a higher-order turbulence closure, with highly simplified background flow. Local te
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| 4. |
- Enger, L, et al.
(författare)
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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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| 5. |
- GRISOGONO, B
(författare)
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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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| 6. |
- Grisogono, B, et al.
(författare)
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Small-scale variability in the coastal atmospheric boundary layer
- 1998
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Ingår i: BOUNDARY-LAYER METEOROLOGY. - : KLUWER ACADEMIC PUBL. - 0006-8314. ; 88:1, s. 23-46
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Tidskriftsartikel (refereegranskat)abstract
- The influence of the main large-scale wind directions on thermally driven mesoscale circulations at the Baltic southwest coast, southeast of Sweden, is examined. The aim of the study is to highlight small-scale alterations in the coastal atmospheric boun
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| 7. |
- Grisogono, B, et al.
(författare)
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Thermal mesoscale circulations on the Baltic coast .2. Perturbation of surface parameters
- 1996
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Ingår i: JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES. - : AMER GEOPHYSICAL UNION. - 0148-0227. ; 101:D14, s. 18999-19012
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Tidskriftsartikel (refereegranskat)abstract
- A three-dimensional numerical study of an observed seabreeze (SE) is presented in a companion paper, part 1. This paper, part 2, addresses the influence of various forcing parameters emanating from the physical surface and perturbing the control run. The
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| 8. |
- GRISOGONO, B
(författare)
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WAVE DRAG EFFECTS IN A MESOSCALE MODEL WITH A HIGHER-ORDER CLOSURE TURBULENCE SCHEME
- 1995
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Ingår i: JOURNAL OF APPLIED METEOROLOGY. - : AMER METEOROLOGICAL SOC. - 0894-8763. ; 34:4, s. 941-954
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Tidskriftsartikel (refereegranskat)abstract
- An incompressible, mesoscale model is used to estimate wave drag (WD) profiles over inhomogeneous 2D terrain. The goal is twofold: to evaluate the WD based on the model's fields and to analyze the atmospheric boundary layer(ABL) response to wave breaking
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| 9. |
- Rogers, David, et al.
(författare)
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Highlights of Coastal Waves 1996
- 1998
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Ingår i: Bulletin of The American Meteorological Society - (BAMS). - 0003-0007 .- 1520-0477. ; 79, s. 1307-1326
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Tidskriftsartikel (refereegranskat)
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| 10. |
- Rogers, DP, et al.
(författare)
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Highlights of Coastal Waves 1996
- 1998
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Ingår i: BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY. - : AMER METEOROLOGICAL SOC. - 0003-0007. ; 79:7, s. 1307-1326
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Tidskriftsartikel (refereegranskat)abstract
- Some of the highlights of an experiment designed to study coastal atmospheric phenomena along the California coast (Coastal Waves 1996 experiment) are described. This study was designed to address several problems, including the cross-shore variability a
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