## Abstract Landโ and seaโbreeze circulations are simulated in a mathematical model, using a stably stratified atmosphere as a basic state. The results show that the landโbreeze is weaker than the seaโbreeze even although the heat contrast at the coast is identical in both cases. This is consistent
A theoretical investigation of the sea breeze
โ Scribed by M. A. Estoque
- Publisher
- John Wiley and Sons
- Year
- 1961
- Tongue
- English
- Weight
- 548 KB
- Volume
- 87
- Category
- Article
- ISSN
- 0035-9009
No coin nor oath required. For personal study only.
โฆ Synopsis
Abstract
A primitive equation model is formulated and integrated numerically to study the sea breeze. The formulation is an extension of an atmospheric boundaryโlayer model previously developed for a homogeneous terrain. External gravityโwave type solutions are suppressed by a modelling assumption involving the equation of continuity. The results of an integration showing the evolution of the sea breeze under conditions of no largeโscale synoptic motion are presented.
๐ SIMILAR VOLUMES
## Abstract The equations of heating and motion are averaged vertically, assuming vertical distributions of velocity and temperature. A nonโlinear partial differential equation of hyperbolic type is found to be satisfied by the surface velocity of the sea breeze. Numerical solutions are given for v
## Abstract Hourly wind speed and direction data from 12 coastline stations on Sardinia, Italy, are analysed in order to characterize sea breezes in the region. A set of criteria based on the diurnal reversal of wind direction, and the thermal gradient necessary to drive the circulation, is used to