Oceanic absorption

Oceanic absorption refers to the process by which the ocean absorbs energy from sunlight and other electromagnetic radiation. The seawater takes in sunlight, particularly in the visible and some infrared wavelengths, converting it into heat. This absorption heats the ocean's upper layers, influencing climate and weather patterns. The amount of absorption depends on factors like water depth, salinity, and impurities. By absorbing solar energy, the ocean acts as a vast heat reservoir, helping regulate global temperatures and driving ocean currents essential for climate stability.