Rainfall runoffs into a nearby body of water, is absorbed by the soil, or is transpired back into the atmosphere.
The majority of nuclear energy on Earth is produced in the core of the sun through nuclear fusion reactions. Once this energy reaches Earth's surface, it is used for electricity generation in nuclear power plants, medical applications such as cancer treatments using radiation therapy, and research purposes like nuclear physics experiments.
The three main influences on the input of solar energy to the Earth are the distance between the Earth and the Sun, the angle at which the sunlight reaches the Earth's surface (known as the solar angle), and the amount of atmosphere the sunlight has to travel through before reaching the Earth's surface. These factors determine the intensity and distribution of solar energy received by different parts of the Earth.
Ultraviolet Types
A map is not a three dimensional representation of earth's surface. The best three dimensional representation of earth's surface is a globe or a topographical map.
The planet with a surface covered three fourths in water and ice is Earth.
Sunlight is composed of three types of ultraviolet (UV) light: UVA, UVB, and UVC. UVA accounts for about 95% of the UV light that reaches the Earth's surface, while UVB makes up the remaining 5%. UVC is absorbed by the Earth's atmosphere and does not reach the surface.
The salt water that covers about three-quarters of the Earth's surface is called the ocean.
water
It either accumulates as snow and ice in the colder parts of the planet, can soak into the ground or run off the surface as rivers in the warmer parts of the planet. The water at the Earth's surface is constantly being circulated in the biosphere of the planet in what is known as the hydrological cycle.
crust mantle core
water
water