The main energy source for heating the ocean and causing ocean currents is the Sun. Solar radiation, in the form of sunlight, is absorbed by the Earth's surface, including both the sea and the land. However, the ocean and land absorb and release this solar energy differently due to their varying physical properties.
In the case of the ocean, water has a high heat capacity, meaning it can absorb and store a large amount of heat energy without significantly changing in temperature. As the Sun's energy is absorbed by the ocean surface, it heats up the water. This heat energy is then distributed and transported by ocean currents, creating large-scale movements of seawater around the globe.
For land, the surface heats up more quickly than water because land has a lower heat capacity than water. Consequently, the land heats up faster during the day and cools down faster at night compared to the ocean. This temperature difference between land and sea contributes to the formation of winds as air moves from areas of high pressure (cool land) to areas of low pressure (warm ocean), creating wind patterns.
In summary, solar radiation from the Sun is the primary source of heat energy that heats up both the sea and the land, driving processes like ocean currents and wind patterns on Earth.
Energy from the sun heats the surface water of the ocean. In tropical regions, surface water can be much warmer than deep water. This temperature difference can be used to produce electricity and to desalinate ocean water. The main source of ocean heat is sunlight. Additionally, clouds, water vapor, and greenhouse gases emit heat that they have absorbed, and some of that heat energy enters the ocean. Waves, tides, and currents constantly mix the ocean, moving heat from warmer to cooler latitudes and to deeper levels. Ocean energy refers to all forms of renewable energy derived from the sea. There are three main types of ocean technology: wave, tidal and ocean thermal. All forms of energy from the ocean are still at an early stage of commercialization. Large-scale surface ocean currents are driven by global wind systems that are fueled by energy from the sun. These currents transfer heat from the tropics to the Polar Regions, influencing local and global climate. Surface currents in the ocean are driven by global wind systems that are fueled by energy from the Sun. Patterns of surface currents are determined by wind direction, Coriolis forces from the Earth's rotation, and the position of landforms that interact with the currents. Besides gravity, the most important forces that cause and affect ocean currents are horizontal pressure-gradient forces, Coriolis forces, and frictional forces. Ocean currents are caused due to uneven heating on the earth's surface; thus, ocean currents will directly affect temperature. For instance, the wind will have a cooling effect when it blows over the cooler parts of the ocean; the surrounding people will feel this impact. Ocean currents transfer heat through convection. Convection is the process of heat transfer by the movement of fluids such as water. When warm liquid is forced to travel away from the heat source, it carries energy with it.Cold-water ocean currents occur when the cold water at the poles sinks and slowly moves towards the equator. Warm-water currents travel out from the equator along the surface, flowing towards the poles to replace the sinking cold water.