Springtide

Springtide is a term used to describe the tidal phenomenon known as a spring tide, in which the gravitational forces of the Moon and Sun combine to produce higher high tides and lower low tides. This alignment occurs during full moon and new moon phases, when the Sun, Moon, and Earth are lined up. The resulting tidal range—the difference between high and low tides—tends to be larger than average. Local tidal patterns are influenced by coastline geometry, ocean floor topography, and sea depth, which can amplify or dampen the effect.

Historically, springtide has appeared as a variant spelling or usage in nautical and historical texts. In contemporary meteorology and oceanography, the standard term is spring tide, though springtide may still be encountered in literature or older sources. The concept is not restricted to any single geographic region and can be observed in coastal areas worldwide, subject to seasonal weather and regional sea conditions.

In culture and nomenclature, Springtide has been adopted as a proper noun in some contexts, including as a name for artistic works, groups, or events, often invoking themes of renewal, growth, and the cyclical nature of tides. The term also figures in poetry and prose where coastal imagery or the idea of a peak moment is central.