The sun and the earth's core.
Geothermal energy is created from the Earth's heat. This renewable energy source harnesses heat from beneath the Earth's surface to generate electricity or provide direct heating.
When Earths surface is heated it radiates some of the energy back into the atmosphere as "Infrared Radiation."
The energy from the sun that is absorbed by the Earth's surface is converted into heat. This heat is then re-radiated back into the atmosphere, contributing to the Earth's overall temperature and driving weather patterns and climate systems.
The two main sources of heat in the troposphere are solar radiation, which warms the Earth's surface, and the release of latent heat energy from water vapor condensing into clouds and precipitation.
The two main sources of Earth's internal heat energy are residual heat from the planet's formation over 4.6 billion years ago and the decay of radioactive isotopes within the Earth's mantle. The heat generated by these processes contributes to the movement of tectonic plates and drives geological activity on the planet.
Because of the heat and light
Sun
Geothermal energy is created from the Earth's heat. This renewable energy source harnesses heat from beneath the Earth's surface to generate electricity or provide direct heating.
The Earth system is powered by energy from two major sources: the Sun and the planet's internal heat.
Energy from the sun that is absorbed by the Earth's surface is reflected back into the atmosphere or absorbed by land and water and transformed into heat.
It is called geothermal energy.
When Earths surface is heated it radiates some of the energy back into the atmosphere as "Infrared Radiation."
Infrared radiation from the sun warms the Earth's surface. This heat energy is then radiated back into space as longwave infrared radiation. This process is known as the greenhouse effect.
The energy from the sun that is absorbed by the Earth's surface is converted into heat. This heat is then re-radiated back into the atmosphere, contributing to the Earth's overall temperature and driving weather patterns and climate systems.
Energy is transferred between the earths surface and the atmosphere via conduction, convection, and radiation. Conduction is the process by which heat energy is transmitted through contact with neighboring molecules.
The two main sources of heat in the troposphere are solar radiation, which warms the Earth's surface, and the release of latent heat energy from water vapor condensing into clouds and precipitation.
How do changes in heat energy affect the density of earths mantle material