The atmosphere reflects some of the energy back into space.
The energy from the sun enters the atmsphere as radiation. This radiation is tranmited to the earth in the form of short waves of radiation. These waves hit the ground.Through radiation.
evaporate water, heat up the atmosphere change the weather e.g. high,low pressure system. used for conversion to electrical energy
Yes
The energy Earth receives from the Sun is often called solar energy. The rate at which this energy arrives at Earth is about 174 petawatts ( 1 petawatt = 1,000 trillion watts) at the upper atmosphere. About 30% is reflected back to space. The sun energy at the Earth's surface is mostly in the visible and near-infrared ranges with a small amount in the near-ultraviolet.
The friction with the Earth's atmosphere causes a meteor to heat up and burn.
kinetic and heat
The earth will become warmer.
The energy from the sun enters the atmsphere as radiation. This radiation is tranmited to the earth in the form of short waves of radiation. These waves hit the ground.Through radiation.
more radiation ; bad living conditions for the people of earth
The sun doesn't heat and power things like weather evenly. Since the Earth is a sphere, different parts of the world absorb heat at different rates. The energy from the sun enters and leaves Earth through absorption.
evaporate water, heat up the atmosphere change the weather e.g. high,low pressure system. used for conversion to electrical energy
more radiation ; bad living conditions for the people of earth
A meteorite.
Yes
When a meteoroid enters the Earth's atmosphere, it is called a meteor. A meteor that passes through the atmosphere and strikes the ground is called a meteorite.
A stone which enters the Earth's atmosphere from outer space is called a meteor.
The energy Earth receives from the Sun is often called solar energy. The rate at which this energy arrives at Earth is about 174 petawatts ( 1 petawatt = 1,000 trillion watts) at the upper atmosphere. About 30% is reflected back to space. The sun energy at the Earth's surface is mostly in the visible and near-infrared ranges with a small amount in the near-ultraviolet.