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- The emissivity of most natural Earth surfaces is a unitless quantity and ranges between approximately 0.6 and 1.0, but surfaces with emissivities less than 0.85 are typically restricted to deserts and semi-arid areas. Vegetation, water and ice have high emissivities above 0.95 in the thermal infrared wavelength range.www.jpl.nasa.gov/images/pia18833-nasa-spacecraft-maps-earths-global-emissi…
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A typical spectrum of infrared radiation transmittance through Earth's atmosphere. A 'window' can be seen between 8 and 14 μm that enables direct transmission of the most intense thermal emissions from Earth's surface. See more
The emissivity of the surface of a material is its effectiveness in emitting energy as thermal radiation. Thermal radiation is electromagnetic radiation that most commonly includes … See more
Emissivities ε can be measured using simple devices such as Leslie's cube in conjunction with a thermal radiation detector such as a See more
The emissivity of a planet or other astronomical body is determined by the composition and structure of its outer skin. In this context, the "skin" of a planet generally includes both its semi-transparent atmosphere and its non-gaseous surface. … See more
Emissivities are important in a variety of contexts:
Insulated windows Warm surfaces are usually cooled directly by air, but they also cool themselves by … See moreIn its most general form, emissivity can be specified for a particular wavelength, direction, and polarization.
However, the most commonly used form of emissivity is the … See moreAbsorptance
There is a fundamental relationship (Gustav Kirchhoff's 1859 law of thermal radiation) that equates the emissivity of a surface with its … See moreWikipedia text under CC-BY-SA license WEBEmissivity, unlike surface temperature, is an intrinsic property of the surface and does not depend on the angle of the sun in relationship to Earth or on local weather conditions. Instead emissivity variations …
WEB[1] Climate models take account of incoming energy from the Sun as well as outgoing energy from Earth. An imbalance results in a change in temperature. The incoming energy from the Sun is in the form of short …
WEBWilliam Brune. Pennsylvania State University via John A. Dutton: e-Education Institute. Let’s first look at the general energy balance—the radiative equilibrium—of the Earth system (see figure below). The solar …
MEaSUREs — Land Surface Temperature and …
WEBLand Surface Temperature and Emissivity (LST&E) data are critical variables for monitoring the long-term effects of climate change and studying a variety of Earth surface processes and surface-atmosphere …
LST/Emissivity Background — Land Surface Temperature and …
Assessment of atmospheric emissivity models for clear-sky
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