As radiation from the sun passes through Earth's atmosphere, it undergoes scattering and absorption by air molecules, water vapor, and aerosols. Some wavelengths, particularly ultraviolet (UV) radiation, are significantly absorbed by the ozone layer, protecting life on Earth. Visible light is mostly transmitted, allowing it to reach the surface. Overall, the atmosphere filters and moderates the amount of radiation that reaches the Earth's surface.
The radiation that passes through the atmosphere and reaches the Earth's surface has the greatest intensity in the form of visible light. This portion of the electromagnetic spectrum, which includes wavelengths from about 400 to 700 nanometers, is crucial for photosynthesis and significantly influences the planet's climate and ecosystems. Ultraviolet and infrared radiation are also present, but they are less intense compared to visible light.
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The Earth's surface transfers heat to the atmosphere primarily by convection and radiation. As the surface heats up, air in contact with the surface warms up and rises, creating vertical currents of warm air. At the same time, the Earth's surface emits radiation in the form of heat, which is absorbed by the atmosphere.
Yes, ultraviolet (UV) radiation can penetrate Earth’s atmosphere, but to varying degrees depending on the wavelength. The atmosphere absorbs most UVC radiation (100-280 nm) and a significant portion of UVB (280-320 nm), but some UVA radiation (320-400 nm) can reach the surface. This is why UV protection is important, as prolonged exposure to UVA can contribute to skin damage and other health issues.
Absorption: Some of the sun's radiation is absorbed by gases such as ozone and water vapor in the Earth's atmosphere. Scattering: Particles in the atmosphere scatter sunlight in all directions, contributing to the blue color of the sky. Reflection: Some of the sunlight is reflected back into space by clouds, aerosols, and the Earth's surface.
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Visible light radiation passes most easily through Earth's atmosphere. This type of radiation includes the colors of the rainbow (RED, ORANGE, YELLOW, GREEN, BLUE, INDIGO, VIOLET).
It absorbs radiation to protect it. It protects from UV rays.
Microwave rays can pass through the Earth's atmosphere, as they are a form of electromagnetic radiation that is not absorbed or blocked by gases in the atmosphere. This is why microwave communication systems like satellites are able to transmit signals through the atmosphere.
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.
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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.
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About 50% of the sun's radiation that reaches Earth's atmosphere is absorbed by the Earth's surface. The remaining energy is either reflected back to space or absorbed by the atmosphere.
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 sun heats the atmosphere. Solar radiation largely passes through the atmosphere and warms the surface of the earth. The earth then radiates heat up into the lower levels of the atmosphere where greenhouse gases warm. The warmed greenhouse gases then continue to radiate heat in all directions warming the atmosphere and again the earth's surface.