White or light coloured surfaces, of which a cloud is an example, reflects sunlight, while dark surfaces absorb sunlight and heats up.
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Clouds reflect sunlight back to space due to their high albedo, or reflectivity. This happens because clouds are made up of tiny water droplets or ice crystals that scatter incoming sunlight. The more dense and widespread the clouds, the more sunlight they can reflect back into space.
Clouds reflect sunlight back to space due to their high albedo, which is the measure of how much sunlight a surface or object reflects. The water droplets or ice crystals in clouds scatter and reflect sunlight, which reduces the amount of solar radiation that reaches the Earth's surface. This reflection plays a role in regulating the Earth's energy balance and helps cool the planet.
Clouds reflect sunlight back into space because of their high albedo, which is a measure of the reflectivity of a surface. The high albedo of clouds is due to their ability to scatter and reflect sunlight, preventing a portion of it from reaching the Earth's surface. This phenomenon has a cooling effect on the Earth's climate by reducing the amount of solar radiation absorbed by the planet.
Clouds reflect and scatter sunlight, reducing the amount of heat that reaches the Earth's surface. They also absorb and trap heat, preventing it from escaping back into space, leading to a cooling effect during the day.
Clouds are an important visible feature of Earth's atmosphere that reflect sunlight back into space. Their brightness and coverage impact the Earth's energy balance and overall climate system.
Clouds can cool down the Earth by reflecting incoming sunlight back into space, which reduces the amount of solar radiation reaching the Earth's surface. They also increase the Earth's albedo, which is its ability to reflect sunlight. Additionally, clouds can trap heat radiated from the Earth's surface, but their overall cooling effect usually outweighs this warming effect.