Roughly 70% of the sun's energy is absorbed by the Earth's surface, with about 51% absorbed by the land and 19% absorbed by the oceans. The absorbed energy is crucial for driving various Earth processes such as weather patterns and the water cycle.
Less than 1% of the Sun's energy is absorbed by Earth's geosphere. The majority of the Sun's energy is absorbed by the atmosphere and surface of the Earth.
To the extent to which the energy is absorbed, yes. Reflectivity and color determine how much energy is absorbed, but no matter can reflect 100% of the energy striking it. Some will be absorbed by the molecules.
One way that land and water differ when it comes to absorbing and losing heat is that water can do so by way of phase change - freezing, melting, evaporating, or condensing. Land tends to stay solid. Water also tends to be much more reflective than land - not always, but in general it is. Land tends to be both a better absorber and radiator of heat.
About 70% of the precipitation that falls on the land originates from the oceans. This water evaporates from the ocean surface, forms clouds, and is transported by atmospheric circulation patterns to eventually fall as rain or snow over land areas.
Roughly 3% of the Sun's energy that reaches the Earth is absorbed by the hydrosphere. This energy plays a crucial role in driving processes like evaporation, which fuel the water cycle that is essential for the Earth's climate system.
About 70% of the solar energy that reaches Earth is absorbed by the land, oceans, and atmosphere. The oceans absorb the largest portion, approximately 50%, while the land and atmosphere together account for the remaining absorption. The absorbed energy drives various processes, including weather patterns, ocean currents, and the overall climate system. The remaining energy is reflected back into space, contributing to Earth's energy balance.
carbon dioxide
The ocean water absorbed much of the carbon dioxide from the atmosphere.
51%
Less than 1% of the Sun's energy is absorbed by Earth's geosphere. The majority of the Sun's energy is absorbed by the atmosphere and surface of the Earth.
Water has a higher specific heat capacity than land (soil, rocks, etc), and also the sun's radiation is not absorbed by water so easily as for land. Similarly for air. Thus the oceans moderate the temperatures reached under sunlight, and the land near the oceans is always cooler than that inland, in summer. In winter though the reverse can be true, because the oceans then become a large store of thermal energy whilst the land cools more quickly in the absence of strong sunlight.
Water has a higher specific heat capacity than land (soil, rocks, etc), and also the sun's radiation is not absorbed by water so easily as for land. Similarly for air. Thus the oceans moderate the temperatures reached under sunlight, and the land near the oceans is always cooler than that inland, in summer. In winter though the reverse can be true, because the oceans then become a large store of thermal energy whilst the land cools more quickly in the absence of strong sunlight.
Water has a higher specific heat capacity than land (soil, rocks, etc), and also the sun's radiation is not absorbed by water so easily as for land. Similarly for air. Thus the oceans moderate the temperatures reached under sunlight, and the land near the oceans is always cooler than that inland, in summer. In winter though the reverse can be true, because the oceans then become a large store of thermal energy whilst the land cools more quickly in the absence of strong sunlight.
Short Answer:Since there is so much more water than land, one expects that most of the solar energy absorbed by Earth is absorbed into the oceans. That is correct.Crudely, twice as much energy is absorbed by the oceans as the land since there is roughly a bit more than twice as much ocean as land.More Technical (Albedo):The characterization of how much solar energy is absorbed by a portion of the surface of the Earth is something called the albedo of the surface. Some surfaces, like dirt, forests and the ocean absorb most of the Sun's energy. Others, like Snow reflect most of it. Deserts are in between.The albedo of a surface is the fraction of light it reflects. (The term "reflects" does not mean like a mirror but rather means scatters or causes to light bounce back to distinguish "reflection" from the process where light is absorbed.) Normally, one refers to sunlight when quoting an albedo, but if a different or specific wavelength range is being considered, there are different values of the albedo that are defined for different parts of the electromagnetic spectrum.On average, the ocean surface has a low albedo meaning it absorbs most of the light that gets to it.The same is true for bare soil and most forests.Though the albedo is variable, 70 or 80 % of the light is absorbed.Desert areas typically have high albedos and can reflect most of the light.Most land areas are in an albedo range of 0.1 to 0.4, so 90% to 60% of the light is absorbed.The average albedo of the Earth is about 0.3, somewhat higher than typical of oceans or much of the land area primarily because of the contribution of clouds.Clouds reflect light very effectively, absorbing little.
20 million metric tons
45%
oceans