Many people know that tides rise and fall as a result of the Moon, but often times people are unaware that the Sun also exerts a tidal force on the Earth. Tides are caused by gravitational force, which depends on the mass of the objects pulling on each other and the distance between them. The moon’s tidal force on Earth is a result of the difference between the gravitational force from the Moon to the near side of Earth and the gravitational force from the Moon to the far side of Earth. This difference creates the tidal force, which caused the whole Earth to behave like a rubber band and stretch to form two bulges (towards and away from the Moon). This means that the part of Earth facing the Moon and the part of Earth facing away from the Moon, experience high tide at the same time. I always assumed that high tide came only when the Moon was out, but this explains why there are two high tides and two low tides per day.
Although these bulges explain daily tides, they do not explain why there is a larger tidal range around New Moons and Full Moons. This is because during those Moon phases the Sun, Earth, and Moon are in a line. The Sun does exert a tidal force on Earth, but it is not as strong as the Moon’s tidal force. The difference between the gravitation force that the Sun exerts on the far side and near side of Earth is very small. This means that the Sun’s tidal force on the Earth is less noticeable on a daily basis, but it is still significant when the Sun and Moon’s tidal forces work together or work against each other. The result of this is spring tides and neap tides.
Spring tides are very high tides or very low tides that happen around Full Moons and New Moons. During these tides the tidal force of the Moon and Sun work together and pull on the Earth in the same direction. During spring tides, there has been a recorded tidal range of up to 16 meters! Neap tides occur around the quarter Moons when the Sun and Moon are at a 90° angle from each other, and therefore pull on different sides of the Earth creating less range between high and low tides.









