(ii) The albedo of Earth appears to be highly buffered on hemispheric and global scales as highlighted by both the hemispheric symmetry and a remarkably small interannual variability of reflected solar flux (~0.2% of the annual mean flux). The Earth's planetary albedo depends mostly on cloud amount and properties, but also on land use. This reflected energy is a fundamental component of the Earth's energy balance, and the processes that govern its magnitude, distribution, and variability shape Earth's climate and climate change. The most recent values obtained are approximately 0.29. The visual albedo of the Earth is 0.37, and the Moon’s is 0.12. Earth albedo is the sunlight reflected off the Earth's surface. For surfaces between the tropics (23.5°N to 23.5°S) the average albedo is 19-38%. The Moon appears darker if the Earth also appears in the same photograph. Visual albedo is the measure of the reflection of solar radiation out of the total solar radiation received by an astronomical body, taking into account only the visible light. We show how clouds provide the necessary degrees of freedom to modulate the Earth’s albedo setting the hemispheric symmetry. The albedo of the Earth is 0.367. Changes in Earth’s surfaces can therefore affect how much of the Sun’s energy is absorbed – such as a decrease in snow cover or an increase in the area used for agriculture. Earth-orbiting satellites have been used to measure Earth’s Bond albedo. Albedo. The lower the albedo, the more energy from the Sun is absorbed. Albedo over UK and Ireland. When Vangelis released his album, Albedo 0.39, that was what the albedo of Earth was in 1976. There is no reason to believe that the planetary albedo has been and will remain constant, and a change of 1% in its value would have a large impact on the Earth's climate system . The Earth albedo induces power in solar cells just like direct sunlight. The fraction of the incoming solar energy scattered by Earth back to space is referred to as the planetary albedo. Albedo is the reflectance of solar energy from the earth’s surface. At the poles, it can be as high as 80% in some areas. The Earth albedo model presented here, calculates the amount of Earth albedo arriving at an object in space, maintaining information of direction of the Earth albedo, useful for objects in low Earth-orbit. Albedo is said to determine the amount of shortwave radiation to be absorbed by surfaces (Vargo et al., 2013). 2.2 Earth's Albedo and Net TOA Solar Radiation above the atmosphere. Flat Earthers use the fact to “prove” that the picture is fake. Like solar radiation in general, albedo values also vary across the globe with latitude but Earth’s average albedo is around 31%. The Moon, which has a very tenuous atmosphere and no clouds, has an albedo of 0.12. By contrast, that of Venus, which is covered by dense clouds, is 0.75.