Land and sea breezes
β Scribed by John Knox Laughton
- Publisher
- John Wiley and Sons
- Year
- 2007
- Tongue
- English
- Weight
- 416 KB
- Volume
- 1
- Category
- Article
- ISSN
- 0035-9009
No coin nor oath required. For personal study only.
π SIMILAR VOLUMES
Sodar measurements have been made at La Spezia, Italy during land-and sea-breeze conditions. The backscatter returns are discussed qualitatively, including their relation to the vertical structure of the boundary layer as revealed by vertical soundings of wind and temperature. During inversion condi
This paper deals with the application of a physically complete land-sea-air boundary layer model for the simulation of flow field and pollutant transport over the Athens basin. As a first approach, a two-dimensional simulation of the tidal air movements in Athens has been performed. Simulation resul
## Abstract Sea/land breezes and inland breezes have in common the βbreezeβ appellation but are essentially different. The land/seaβbreeze horizontal extent exceeds 100 km, with the Coriolis effect dominating its dynamics. Conversely, inland breezes are confined between alternating patches of cold
## Abstract Landβ and seaβbreeze circulations are simulated in a mathematical model, using a stably stratified atmosphere as a basic state. The results show that the landβbreeze is weaker than the seaβbreeze even although the heat contrast at the coast is identical in both cases. This is consistent