During a spring tide, the sun, moon, and Earth align in a straight line, which occurs during full and new moons. This alignment causes the gravitational forces of the sun and moon to work together, resulting in higher high tides and lower low tides. Consequently, the tidal range—the difference between high and low tide—is greater than during other phases of the moon. This phenomenon exemplifies how the celestial arrangement can significantly influence tidal patterns.
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