The earth's energy is in balance, meaning there is about as much going out as there is coming in. This keeps the earth's climate roughly in equilibrium. If there were more coming in than release, this would invariably warm the earth's atmosphere.
This is called the "albedo." It is the ratio of reflected light compared to incident light, and depends on the surface material and its condition (e.g. snow, grassland).
The atmosphere is heated chiefly by radiation from Earth's surface rather than by direct solar radiation because about 50 percent of the solar energy is absorbed at Earth's surface. 30 percent is reflected back to space. 20 percent is absorbed by clouds and the atmosphere's gases.
Solar radiation is absorbed by Earth's atmosphere, surface, and oceans. Some of it is reflected back into space, some is absorbed and later re-emitted as heat, and some is converted into chemical energy through photosynthesis by plants. Some is also reflected directly back into space by clouds, snow, ice, and other reflective surfaces.
Sunlight gets absorbed, scattered, reflected, and transmitted through the atmosphere. Almost all of the ultraviolet component gets absorbed by ozone in the stratosphere. About half of the radiation gets absorbed or scattered and reflected in the troposphere. The remainder passes through, getting absorbed by the earth's surface.
Over half is either reflected, deflected or absorbed as it enters our atmosphere. Of the remaining 47% that hits our planet, most is reflected as visible light and passes through the atmosphere and out into space. Some energy is absorbed by the planet and released as infrared radiation. A small portion of this is absorbed by water vapor and CO2 and is released at night to keep the planet warm and alive.
About 6% of incoming solar radiation is reflected back into space from the atmosphere and 4% by the surface of the earth.Incoming solar radiation: 100%Reflected by the atmosphere: 6% : Absorbed by the atmosphere: 16%Continuing incoming solar radiation: 78%Reflected by clouds: 20% : Absorbed by clouds: 3%Continuing incoming solar radiation: 55%Reflected by the earth's surface: 4% : Absorbed by the earth's surface (lands and oceans): 51%
About 6 percent of solar radiation is absorbed by the Earth's surface, with the remaining percentage being reflected back into space or absorbed by the atmosphere.
Solar radiation that is not reflected is absorbed by clouds, the atmosphere and the surface of the earth.Incoming solar radiation: 100%Reflected by the atmosphere: 6% : Absorbed by the atmosphere: 16%Continuing incoming solar radiation: 78%Reflected by clouds: 20% : Absorbed by clouds: 3%Continuing incoming solar radiation: 55%Reflected by the earth's surface: 4% : Absorbed by the earth's surface (lands and oceans): 51%Source: (NASA)
When radiation hits Earth's surface, it can be absorbed, reflected, or scattered. Some of the absorbed radiation warms the surface, causing temperatures to increase, while some is re-radiated back into the atmosphere as heat. The remaining radiation is reflected back into space, contributing to Earth's energy balance.
When radiation reaches Earth's surface, it can be absorbed, reflected, or scattered. The amount of radiation that is absorbed can contribute to heating of the surface and atmosphere. This process is fundamental for maintaining Earth's energy balance and climate.
Gamma radiation can be both absorbed and reflected. The amount that is absorbed or reflected depends on the material and thickness it interacts with. Some materials like lead are good for absorbing gamma radiation, while others like concrete are better for reflecting it.
The shortwave radiation that reaches Earth's surface and is not reflected is absorbed by the surface, warming it up.
This absorbed energy is then re-radiated as heat
Approximately 51% of incoming solar radiation is absorbed by Earth's surface. The rest is reflected back into space or absorbed by the atmosphere.
About 19% of incoming solar radiation is absorbed by clouds and the atmosphere.Incoming solar radiation: 100%Reflected by the atmosphere: 6% : Absorbed by the atmosphere: 16%Continuing incoming solar radiation: 78%Reflected by clouds: 20% : Absorbed by clouds: 3%Continuing incoming solar radiation: 55%Reflected by the earth's surface: 4% : Absorbed by the earth's surface (lands and oceans): 51%Source: (NASA)
This isn't the best answer, but it starts with 100% radiation, 25% is reflected back by clouds and other particles, 20% is absorbed by particles in the atmosphere, 50% of radiation reaches and is absorbed by Earth's surface, and 5% of radiation from the sun is reflected by land and sea surface.
UV light is absorbed by the ozone layer. It is the harmful part of sun's radiation.