The answe to this question is false. Long-wave radiation from the ground does not pass through the atmosphere without absorption.
Longwave radiation can pass through glass, as glass is transparent to certain wavelengths of energy. However, glass has some absorptive properties, so some of the longwave radiation may be absorbed and re-emitted as heat within the glass. This can contribute to the warming effect inside a greenhouse or a car on a sunny day.
Heat energy is transferred through the atmosphere by conduction, convection, and radiation. Conduction occurs when heat is transferred through direct contact between molecules. Convection is the transfer of heat through the movement of air or fluid, while radiation involves the emission and absorption of electromagnetic waves.
Air density affects the absorption and radiation of energy by determining how easily heat can be transferred through the atmosphere. Lower air density reduces the efficiency of energy absorption and radiation. Elevation plays a crucial role as higher elevations have lower air density, which can result in reduced energy absorption and radiation compared to lower elevations.
The troposphere and thermosphere are the layers of the atmosphere where most of the energy transfer occurs. In the troposphere, heat is transferred through processes like convection and radiation, while in the thermosphere, energy is primarily transferred through absorption of solar radiation.
No, radiation from the sun heats the Earth primarily through the process of absorption of solar radiation by the Earth's surface and atmosphere. Convection is the transfer of heat through the movement of fluids, such as air and water, but it is not the primary mechanism by which the Earth is heated by solar radiation.
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.
Some processes that help balance the heat budget of Earth's surface include radiation from the sun warming the surface, heat transfer through conduction and convection, and the reflection and absorption of heat by clouds and greenhouse gases. The Earth's surface also releases heat back into the atmosphere through processes like longwave radiation and latent heat transfer.
Longwave radiation can pass through glass, as glass is transparent to certain wavelengths of energy. However, glass has some absorptive properties, so some of the longwave radiation may be absorbed and re-emitted as heat within the glass. This can contribute to the warming effect inside a greenhouse or a car on a sunny day.
The troposphere and stratosphere are responsible for the majority of solar radiation absorption in the atmosphere. The troposphere absorbs most of the incoming solar energy through the greenhouse effect, while the stratosphere absorbs ultraviolet radiation from the sun through the ozone layer.
The process of longwave radiation trapping through the greenhouse effect has the greatest role in warming the upper troposphere. Greenhouse gases, such as carbon dioxide and water vapor, trap outgoing longwave radiation, leading to a warming effect in the upper troposphere. This process is critical for maintaining Earth's temperature and climate.
Solar radiation leaves Earth's atmosphere through a process called reflection and absorption. Some of the radiation is reflected back into space by clouds, gases, and particles in the atmosphere. The remaining radiation is absorbed by the surface of the Earth, where it is converted into heat energy.
No, UVC radiation is mostly absorbed by the Earth's atmosphere, particularly by the ozone layer. This absorption helps to protect living organisms on Earth from the harmful effects of UVC radiation.
The greenhouse effect occurs when certain gases in the Earth's atmosphere, like carbon dioxide and methane, trap longwave radiation (heat) from the sun. These gases allow sunlight to pass through and warm the Earth's surface, but they prevent some of the heat from escaping back into space. This trapped heat warms the planet, similar to how a greenhouse traps heat to keep plants warm.
Carbon dioxide mainly has an effect on longwave radiation. It absorbs longwave radiation and re-radiates it, some of it back downwards. This means carbon dioxide increases the amount of radiation going back down to the surface, and the surface has to warm up to compensate.
Roughly 20% of visible light radiation is absorbed as it passes through the Earth's atmosphere. The remaining percentage is either reflected back into space or reaches the Earth's surface. This absorption is influenced by factors such as cloud cover, aerosols, and gases in the atmosphere.
Heat energy is transferred through the atmosphere by conduction, convection, and radiation. Conduction occurs when heat is transferred through direct contact between molecules. Convection is the transfer of heat through the movement of air or fluid, while radiation involves the emission and absorption of electromagnetic waves.
Air density affects the absorption and radiation of energy by determining how easily heat can be transferred through the atmosphere. Lower air density reduces the efficiency of energy absorption and radiation. Elevation plays a crucial role as higher elevations have lower air density, which can result in reduced energy absorption and radiation compared to lower elevations.