Température de la mer autour du Massif armoricain selon les données du satellite NOAA/AVHRR

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Abstract
The temperature of the sea surface, TSS, around the Massif Armoricain, studied for some sunny days on the Channel, and on the Golfe de Gascane from NOAA-A VHRR, data appliing the algorithm created by the CMS of Lannion. The analysis of these situations points out show the interactions between the local aspects of the energy balance, the atmospheric circulation and the oceanic hydrology to explain the seasonal inversion of the spatial distribution TSS from the coast of Leon at the Gulf of Saint-Malo and the sudder heating of the littoral oceanic waters, in the spring and at the beginning of the sommer. Today, it is not possible to limit only the influence of the warm waters of the Gulf Stream (or northen-atlantic drift) to understand the climates of this coastal line.

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