Spring tides occur during new and full moons when the sun and moon are aligned, causing their tidal bulges to constructively interfere and produce the largest difference between high and low tides. Neap tides happen at quarter moons when the sun and moon are at right angles, causing their tidal bulges to destructively interfere and result in a smaller tidal range. The tidal range is greatest when the moon is closest to Earth at perigee and Earth is closest to the sun at perihelion.