Radiation budget is Earth's atmosphere. The Earth's atmosphere has more solar energy than it radiates back to space.
The total amount of energy coming into and leaving the atmosphere is referred to as Earth's energy budget. It includes incoming solar radiation and outgoing terrestrial radiation. This balance of energy is crucial for maintaining Earth's temperature and climate.
The solar energy absorbed by Earth is primarily radiated back into space as infrared radiation. After the Earth's surface absorbs sunlight, it warms up and emits energy in the form of longwave infrared radiation. This process helps regulate the planet's temperature and maintain a balance in the Earth's energy budget.
The region near the equator receives the most solar radiation because it receives sunlight more directly throughout the year due to the Earth's tilt and position in its orbit. This area, known as the tropics, receives the highest intensity of sunlight, making it ideal for solar energy generation.
zeta radiation [Adam strange] is a type of radiation yhat interstellarly telaports you from planet to planet
hey yall this isd tay taaaaaaayy,,,, the answer is ultra violet radiation
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It's actually the rain forest because that is the biome closest to the equator, meaning that it has a net radiation budget surplus (more solar radiation is absorbed than reflected/re-emitted as infrared radiation), unlike the biomes closer to the poles which will have a net radiation budget deficit (more infrared radiation is re-emitted/reflected than solar radiation that is absorbed).
It's actually the rain forest because that is the biome closest to the equator, meaning that it has a net radiation budget surplus (more solar radiation is absorbed than reflected/re-emitted as infrared radiation), unlike the biomes closer to the poles which will have a net radiation budget deficit (more infrared radiation is re-emitted/reflected than solar radiation that is absorbed).
G. Louis Smith has written: 'Atlas of albedo and absorbed solar radiation derived from Nimbus 7 earth radiation budget data set, November 1978 to October 1985' -- subject(s): Albedo, Charts, diagrams, Heat budget (Geophysics), Measurement, Measurrement, Nimbus (Artificial satellite), Terrestrial radiation 'Atlas of albedo and absorbed solar radiation derived from Nimubs 6 earth radiation budget data set - July 1975 to May 1978' -- subject(s): Albedo, Earth radiation budget, Solar radiation
Long wave radiation in the Earth's energy budget primarily comes from the Earth's surface. The surface absorbs shortwave radiation from the sun and then emits longwave radiation back into the atmosphere. This longwave radiation plays a crucial role in maintaining the Earth's energy balance.
It's because of radiation that as you know black body is an ideal radiation body for good radiation and so good heat transfer.
The reason with the greatest deficit in its net radiation budget is typically associated with areas that experience high albedo, such as polar regions covered in ice and snow. These surfaces reflect a significant portion of incoming solar radiation rather than absorbing it, leading to lower net radiation. Additionally, regions with persistent cloud cover can also contribute to a negative net radiation budget by blocking sunlight and trapping heat, further exacerbating the deficit.
Scientists can determine the Earth's heat budget by measuring incoming solar radiation and outgoing thermal radiation. If more energy is absorbed than emitted back into space, it indicates an imbalance in the Earth's heat budget. This imbalance can lead to global warming and climate change.
The emissivity of an ideal reflector is 0, meaning it reflects all incoming radiation without emitting any.
If Earth's net radiation budget became unbalanced, it could lead to changes in the planet's temperature and climate. If incoming solar radiation exceeds outgoing heat radiation, Earth would warm, potentially causing global warming and climate change. Conversely, if outgoing heat radiation exceeds incoming solar radiation, Earth would cool, possibly leading to a global cooling event.
Sally Ride and Marc Gameau helped to deploy the Earth Radiation Budget Satellite in 1984. It launched from Kennedy Space Center on October 5th, 1984.
It's shielded from radiation. It has water. It has oxygen.