The horizontal distribution of temperature in the oceans refers to the variation in sea surface temperature from one place to another across different latitudes and longitudes. It is influenced by several physical and climatic factors that determine the amount of heat received, retained, and transported by ocean waters. Among these, latitude and ocean currents are the two most significant factors affecting the horizontal distribution of ocean temperature. Latitude is the primary factor controlling the horizontal distribution of ocean temperature because it determines the angle at which solar radiation reaches the Earth's surface. Near the Equator, the Sun's rays fall almost vertically throughout the year, resulting in