Definition:
Mouvement horizontal côtier de la mer provoqué alternativement par la marée montante (le flot) et la marée descendante (le jusant). Les cours d’eau qui sont hydrauliquement reliés à la mer peuvent se saliniser et voir leur courant s’inverser selon la marée.
Source:
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Food and Agriculture Organization of the United Nations, AQUASTAT Web Site
AQUASTAT. 2008. Adapted from FAO glossary