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...and [[dissipation]] of [[energy]] in the [[Atmospheric circulation|general atmospheric circulation]].<ref name="HoltonDynMet">{{cite book|last1=Holton|first1=Jame Any atmospheric circulation system, whether it is a small-scale [[weather]] system or a [[P ...

...[Sunlight|solar radiation]] and partially absorbing of [[Infrared|infrared radiation]] from the planet. It provides an approximation for the temperature of the ...energy fluxes exchanged between layers, and dotted lines indicate that the radiation passes through one or more layers. Note that the flux radiated upwards by t ...

It is used very commonly in the [[geoscience]]s, particularly for [[atmospheric sounding]]. ...tmospheric Temperature and Composition From Remote Measurements of Thermal Radiation ...

...al cloud datasets from satellites: Project and Database initiated by GEWEX Radiation Panel [[Category:Atmospheric sciences]] ...

...surface to another is the equal to the difference of incoming and outgoing radiation from the first surface. In general, the heat transfer between surfaces is g ...not depend upon the media. Because media neither absorb, emit, nor scatter radiation. ...

...'s radiation balance with its parent star and the rest of space. Thermal radiation absorbed and emitted by the idealized atmosphere can raise the equilibrium ...''leave''. Rather than get hotter and hotter, [[Kirchhoff's law of thermal radiation]] says that the gases of the atmosphere also have to re-emit the infrared e ...

...otal [[thermal radiation]] leaving an object is equal to the total thermal radiation entering it. It is one of the several requirements for [[thermodynamic equi ...that each body radiates to, and receives radiation from, other bodies. The radiation from each body is emitted regardless of the presence or absence of other bo ...

...er. McGraw-Hill, 1967.</ref><ref>Sparrow, Ephraim M., and Robert D. Cess. "Radiation heat transfer." Series in Thermal and Fluids Engineering, New York: McGraw- ...

...related to the wavelength of radiation? &#124; METEO 300: Fundamentals of Atmospheric Science }}</ref> The photon energy of near [[infrared]] radiation at 1&nbsp;μm wavelength is approximately 1.2398&nbsp;eV. ...

...er. McGraw-Hill, 1967.</ref><ref>Sparrow, Ephraim M., and Robert D. Cess. "Radiation heat transfer." Series in Thermal and Fluids Engineering, New York: McGraw- ...

...ncy (<math>\omega^2</math>). Scattered waves are emitted in a short dipole radiation pattern.<ref name=":02" /> The variable phase shift present in semi-collisi ...thumb|Electron Motion in a Plasma Object During One Half-Cycle of Incident Radiation]] ...

...ism|classical electromagnetic radiation]] of any kind, including [[thermal radiation]] and [[light]]. It is conceptually distinct from the descriptions in expli ...}}, page 16.</ref><ref>Liou, K.N. (2002). ''An Introduction of Atmospheric Radiation'', second edition, Academic Press, Amsterdam, {{ISBN|978-0-12-451451-5}}, p ...

...y (CVAO) at [[São Vicente (Cape Verde)|São Vicente]], [[Cape Verde]]]]In [[atmospheric chemistry]], '''differential optical absorption spectroscopy (DOAS)''' is u The change in intensity of a beam of radiation as it travels through a medium that is not emitting is given by [[Beers law ...

...d both receive and emit in this wavelength; the warmer the Earth, the more radiation it emits. Thus changes in the albedo may have an effect on Earth's temperat ...n some narrow parts of the spectrum this is not so; doubling the amount of atmospheric carbon dioxide will make Earth's atmosphere relatively opaque to in these w ...

...constant—that is, unchanging—for all frequencies of the star's incident [[radiation]]. ...tes from observational results because real atmospheres are not grey, e.g. radiation absorption is frequency-dependent. ...

...edium]] in local [[thermodynamic equilibrium]] that both absorbs and emits radiation. ...ar|dI_λ}}, [W/sr/m²/μm]) at a given [[wavelength]] as radiation travels an incremental distance ({{mvar|ds}}) through a non-[[optical scatt ...

...e. Even small changes in the skin temperature can lead to large changes in atmospheric circulation. This makes skin temperature a widely used quantity in weather ...servation, cloud/snow differentiation, surface temperature observation and atmospheric correction.<ref name=":2" /> The modern satellite array is able to give a g ...

...fficient can be used to help characterize the solar spectrum after [[solar radiation]] has traveled through the atmosphere. The overall intensity of solar radiation is like that of a [[black body]] radiator of the same size at about 5,800&n ...

...d J. |last2=Zeng |first2=Xiping |date=2005-04-01 |title=Modelling tropical atmospheric convection in the context of the weak temperature gradient approximation |u ...title=A Note on Large-Scale Motions in the Tropics |journal=Journal of the Atmospheric Sciences |language=EN |volume=20 |issue=6 |pages=607–609 |doi=10.1175/1520- ...

...allace |Hobbs |2006 |pp=119–120}} The '''[[effective temperature|effective radiation emission temperature]]''' is a related concept,<ref>Stull, R. (2000). ''Met ...and therefore only absorbs a fraction of radiation. The planet absorbs the radiation that isn't reflected by the albedo, and heats up. One may assume that the p ...