Last Updated:2025/11/19
A high tide in which the water rises to a given level, recedes, and then rises again. / A low tide in which the water recedes to a given level, rises, and then recedes again.
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Source Word
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Noun
historical
Japanese Meaning
潮位が所定の水準まで上昇した後、一度水位が下がり、再び上昇する満潮現象 / 潮位が所定の水準まで低下した後、一度水位が上昇し、再び低下する干潮現象
( plural )