Radiated away as heat. If the Earth lost energy constantly, it would eventually freeze; if it gained energy constantly, it would eventually boil. The Earth has an energy balance; equal amounts of energy are absorbed by the Earth as sunlight as are radiated away as heat.
If the Earth were to become too warm, more clouds would form, reflecting light away and causing the Earth to cool down. If the Earth were to get too cold, fewer clouds would form, allowing more heat and light in. However, over the past few million years, the Earth has had more ice ages than moderate periods.
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∙ 14y agoEventually all the energy that reaches the Earth's surface is either reflected back into space, absorbed by the atmosphere, or absorbed by the Earth's surface.
50%
What happens to Solar Energy is that some of it gets absorbed into air, land and water while the rest gets reflected back to space.
Geothermal energy reaches Earth's surface through the Earth's core, where temperatures are extremely high due to the heat generated by radioactive decay. This heat is transferred through rocks and magma in the Earth's mantle, eventually reaching the surface in the form of volcanic activity, geysers, and hot springs.
Most solar energy that reaches Earth's atmosphere is absorbed by the surface of the Earth, such as the land, oceans, and vegetation. This absorption heats up the Earth's surface and is then radiated back into the atmosphere as heat energy.
Roughly 70% of the solar energy that reaches the outer atmosphere is absorbed by the Earth's surface. The remaining percentage is reflected back into space by clouds, aerosols, and the Earth's surface.
50%
About 50% of the sun's radiation that reaches Earth's atmosphere is absorbed by the Earth's surface. The remaining energy is either reflected back to space or absorbed by the atmosphere.
What happens to Solar Energy is that some of it gets absorbed into air, land and water while the rest gets reflected back to space.
The Earth's surface is heated by the sun through a process called solar radiation. Sunlight, which consists of energy in the form of electromagnetic waves, reaches the Earth and heats up its surface when it is absorbed by land, water, and other surfaces. This energy is then retained and warms the Earth's surface.
The Earth looks bright - thus much of the light reaching Earth is reflected back into space.
The amount of radiation absorbed by the Earth's surface varies depending on factors such as location, time of day, and cloud cover. On average, about half of the solar radiation that reaches the Earth's atmosphere is absorbed by the surface, where it is then transformed into heat energy.
The primary factor that affects the amount of solar energy reaching any point on Earth's surface is the angle at which the sunlight hits the surface. This angle, known as the solar zenith angle, determines the path length through the atmosphere that the solar radiation must travel, affecting the amount of absorption and scattering that occurs. The higher the angle, the more direct the sunlight, and the more energy that reaches the surface.
the greenhouse effect!
the greenhouse
epicenter
its about just 1%
They absorb radiant energy emitted by Earths surface