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- W1843281118 abstract "Publisher Summary This chapter reviews the aspects of the Liguro-Provencal frontal ecohydrodynamics. The dynamics of the Mediterranean Sea is mainly dominated by the general and the local atmospheric forcing. Because of the climatology of the Mediterranean area, the water balance is negative, the evaporation being more important than the precipitations and the river supply. In this concentration basin, the deficit is compensated for by an important water flux through the Gibraltar Strait. The Atlantic surface layer flows eastwards along the North African coast, forming the African current. In the western part of the Mediterranean large cyclonic circulations are developed in the Thyrrhenian Sea and in the Liguro-Provencal basin. In addition, the study of hydrological data collected in March, July and October 1984, during several oceanographic cruises across the Ligure-Provencal front (Corsican area), provides a more detailed picture of water masses distribution and seasonal fluctuations." @default.
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- W1843281118 date "1986-01-01" @default.
- W1843281118 modified "2023-09-25" @default.
- W1843281118 title "Some Aspects of the Liguro-Provencal Frontal Ecohydrodynamics" @default.
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- W1843281118 doi "https://doi.org/10.1016/s0422-9894(08)71048-1" @default.
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