water vapor
Carbon dioxide (CO2) is the most powerful absorber of radiation emitted by Earth among greenhouse gases. It contributes significantly to the greenhouse effect and plays a key role in regulating Earth's temperature.
Greenhouse gases absorb shortwave radiation by allowing it to pass through the Earth's atmosphere and reach the surface. Once the radiation hits the surface, it is absorbed and re-emitted as longwave radiation. Greenhouse gases then trap this longwave radiation, preventing it from escaping back into space and causing the Earth's temperature to rise.
Infrared radiation is the type of radiation trapped in the atmosphere due to greenhouse gases. This radiation is emitted by the Earth's surface and is absorbed and re-radiated by greenhouse gases, such as carbon dioxide and water vapor, leading to the warming of the Earth's surface.
Longwave radiation refers to infrared radiation emitted by the Earth's surface and atmosphere, which can be absorbed by greenhouse gases and contribute to warming the atmosphere. Shortwave radiation, such as sunlight, is absorbed by the Earth's surface and then re-emitted as longwave radiation. This difference in wavelengths affects how energy is distributed in the atmosphere, with longwave radiation playing a key role in the greenhouse effect and shortwave radiation driving the Earth's climate system.
Long wavelength radiation, such as infrared radiation, is emitted by Earth's surface after absorbing solar radiation. Greenhouse gases in the atmosphere trap this long wavelength radiation, leading to a warming effect known as the greenhouse effect. This process helps regulate Earth's temperature by keeping the planet warm enough to support life.
Carbon dioxide (CO2) is the most powerful absorber of radiation emitted by Earth among greenhouse gases. It contributes significantly to the greenhouse effect and plays a key role in regulating Earth's temperature.
In terms of total absorbtion, it is water vapor. It absorbs around 75 to 80% of all the heat the atmosphere absorbs in total. Second place is CO2 which takes in around 5% of all warmth.
Infrared radiation is the type of radiation that gets trapped on Earth's surface by the greenhouse effect. This radiation is emitted by the Earth's surface in response to the incoming solar radiation and is absorbed and re-emitted by greenhouse gases in the atmosphere, leading to the warming of the planet.
Greenhouse gases primarily trap infrared radiation emitted by the Earth's surface. When sunlight reaches the Earth, it is absorbed and re-emitted as infrared radiation. Greenhouse gases, such as carbon dioxide and methane, absorb some of this infrared radiation and re-radiate it in all directions, including back towards the Earth's surface, contributing to the greenhouse effect and warming the atmosphere.
Greenhouse gases absorb shortwave radiation by allowing it to pass through the Earth's atmosphere and reach the surface. Once the radiation hits the surface, it is absorbed and re-emitted as longwave radiation. Greenhouse gases then trap this longwave radiation, preventing it from escaping back into space and causing the Earth's temperature to rise.
water vapor. These gases are greenhouse gases that absorb and re-emit the infrared radiation emitted by the Earth's surface, trapping heat in the atmosphere and leading to the greenhouse effect.
Infrared radiation is the type of radiation trapped in the atmosphere due to greenhouse gases. This radiation is emitted by the Earth's surface and is absorbed and re-radiated by greenhouse gases, such as carbon dioxide and water vapor, leading to the warming of the Earth's surface.
Greenhouse gases help trap infrared radiation in the atmosphere. This type of radiation is emitted by the Earth's surface after it absorbs energy from sunlight. By retaining this heat, greenhouse gases contribute to the greenhouse effect, which warms the planet. This process is crucial for maintaining a stable climate but can lead to global warming when excessive greenhouse gases accumulate.
Greenhouse gases in the Earth's atmosphere absorb infrared radiation emitted by the Earth's surface. This absorption traps heat in the atmosphere, leading to the warming of the Earth's surface. This process is known as the greenhouse effect.
Longwave radiation refers to infrared radiation emitted by the Earth's surface and atmosphere, which can be absorbed by greenhouse gases and contribute to warming the atmosphere. Shortwave radiation, such as sunlight, is absorbed by the Earth's surface and then re-emitted as longwave radiation. This difference in wavelengths affects how energy is distributed in the atmosphere, with longwave radiation playing a key role in the greenhouse effect and shortwave radiation driving the Earth's climate system.
terestrial
This powerful energy is likely referring to nuclear radiation emitted by radioactive heavy atoms, such as uranium or plutonium. This radiation can take the form of alpha particles, beta particles, or gamma rays, and can be harmful to living organisms if not properly contained or shielded against.