The atmospheric flow generated in response to horizontal gradients in the surface temperature or heatflux is investigated. A linear model is described that can treat the problem for the case of small surface temperature gradients, including the approximate effect of a large-scale flow and the effect of a vertical structure in the heat and momentum diffusivity, and in the stratification. The second part of this report describes a numerical mesoscale model, and results from the application of this model to the simulation of the sea-breeze.
| Series | Risø-R |
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| Number | R-452 |
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| ISSN | 0106-2840 |
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