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A rip current, a tide, is formed at low tide,
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Rip current in the Caspian Sea. https://en.m.wikipedia.org/wiki/Rip_current A rip current, a tide, is formed at low tide, when the water begins to move (at different speeds) back to the sea. The amplitude of the rip current depends on the speed of the current along the coast. And the speed of the current along the coast depends on the speed and direction of the wind along the coast and the amount of water flowing into the Caspian Sea from the Volga River. Knowing the speed of the current along the coast, it is possible to predict the rip current with an accuracy of up to a minute. http://tapemark.narod.ru/more/06.pngThe shallower the coast, the faster the speed of the current along the coast. In summer, during floods in the Volga River, the amplitude of the rip current is maximum, in spring, autumn and during drought in the Volga River basin it is minimal. The cause of the formation of a rip current may also be a surge wave. https://en.m.wikipedia.org/wiki/Storm_surge Continuation: Academgorodok Forum Novosibirsk. The science. https://forum.academ.club/index.php?showtopic=1235578