Most fuel for heating is from fossil fuels such as oil, coal, and natural gas.
The Earth gets most of its heat from the sun. Solar radiation warms the surface of the Earth, which in turn heats up the atmosphere. Additionally, heat from the Earth's core, known as geothermal heat, also contributes to the overall temperature of the planet.
Most of Earth's heat comes from the Sun, which radiates energy in the form of sunlight. This energy is absorbed by the Earth's surface, leading to warming of the planet. Additionally, a small portion of the Earth's heat also comes from the radioactive decay of elements in the Earth's core.
The most effective greenhouse gas for trapping heat in the Earth's atmosphere is carbon dioxide (CO2).
Most of the energy that heats Earth's atmosphere comes from the sun. Solar radiation warms the Earth's surface, which then radiates heat back into the atmosphere, creating temperature variations and weather patterns.
The Earth is primarily heated from the top by the Sun's radiation. The atmosphere then traps some of this heat, creating the greenhouse effect which warms the surface of the Earth. Heat from the Earth's core also contributes to the planet's overall temperature, however, most of this heat is dissipated through the Earth's crust and is not a primary heat source for the surface.
in the heat inside the earth
The Earth gets most of its heat from the sun. Solar radiation warms the surface of the Earth, which in turn heats up the atmosphere. Additionally, heat from the Earth's core, known as geothermal heat, also contributes to the overall temperature of the planet.
the core
the Sun
Most of Earth's heat comes from the Sun, which radiates energy in the form of sunlight. This energy is absorbed by the Earth's surface, leading to warming of the planet. Additionally, a small portion of the Earth's heat also comes from the radioactive decay of elements in the Earth's core.
The most effective greenhouse gas for trapping heat in the Earth's atmosphere is carbon dioxide (CO2).
True. The majority of Earth's heat is stored in the mantle, which is the layer of Earth located between the crust and the core. This heat is generated by the decay of radioactive elements and leftover heat from the planet's formation.
Infrared light delivers most of the heat from the sun to the Earth. This type of light has longer wavelengths than visible light and is able to penetrate the Earth's atmosphere more effectively, transferring its energy into heat when absorbed by surfaces on the Earth's surface.
The heat is still rising from the main source, the interior of the Earth, where massive pressures, radioactive decay, and leftover heat from Earth's formation is insulated by the mass of the Earth. The heat eventually dissipates into the atmosphere and space. In time, the Earth will cool and most geologic processes will stop.
Heat!!!!!! While the sun does produce a lot of heat, none of it reaches Earth. What reaches Earth is electromagnetic energy (light). Some of this light is converted to heat here on Earth, such as some of the light that hits your skin.
Heat.
water air heat