Definición:
Movimiento horizontal del mar en la costa causado alternativamente por la marea alta y la marea baja. Los ríos que están conectados hidráulicamente al océano pueden salinizarse o incluso invertir el sentido de su caudal en función de la marea.
Fuente:
Food and Agriculture Organization of the United Nations, AQUASTAT Web Site
AQUASTAT. 2008. Adapted from FAO glossary
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Términos Relacionados:
En Glosario Aquastat: Agua salobre, Río
En Glosario de Riego: corriente, salinización