Throughout the day, tides, continuously, rise, or fall. When the water is at its highest, it's called high tide. This phenomenon is explained by the science of Oceanography.
Throughout the day, the continuous gravitational interaction between the Moon and Earth results in the fascinating phenomenon of ocean tides.
As the Moon orbits the Earth, its gravitational pull varies based on its position relative to the Sun. When the gravitational force from the Moon aligns with that of the Sun, during a new or full moon, tidal forces are strengthened, leading to higher high tides and lower low tides—this is known as spring tide.
In contrast, when the Sun and the Moon are at right angles, during the first and third quarters of the moon, tidal forces partially cancel each other out, resulting in lower high tides and higher low tides—this is called neap tide.
Throughout this tidal cycle, water levels continuously rise and fall, creating the rhythmic ebb and flow of the tides. The study of these tidal phenomena, their patterns, and their impact on coastal ecosystems falls under the scientific discipline of Oceanography.
When the water is at its highest point in this tidal oscillation, it is termed "High Tide." Understanding these tidal patterns is not only crucial for scientific exploration but also has practical implications for coastal communities, navigation, and various marine activities.