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...ith atmospheres denoting an imbalance between surface radiation and top-of-atmosphere radiation due to the presence of greenhouse gases.

Second major layer of Earth's atmosphere, just above the troposphere, and below the mesosphere, stratified in temper

...ss of [[water]] droplets, or frozen crystals of water, suspended in the [[atmosphere]] at or close to the [[Earth]]'s surface.

...llites in [[satellite orbits|Earth orbits]] but potentially a relay in the atmosphere

...o the soil, is changed chemically by various processes, and returns to the atmosphere once again. This cycle is necessary for life on earth.

Layer of the earth's atmosphere, directly above the mesosphere and directly below the exosphere, where ultr

The [[gas]] that exits to the atmosphere via a ''flue'' which may be a pipe, channel or chimney for conveying [[comb

...rbital vehicle to reenter the atmosphere, or, especially in the absence of atmosphere, braking a space vehicle to a "soft" landing. Some have been used to brake

...') that is equal to ¹/₇₆₀ of an [[Atmosphere (unit)|atmosphere]] (symbol: '''atm''').<ref name=TorrName group=note/> It was selected to be ...the height needed for a water barometer. That, in effect, proved that the atmosphere did indeed have weight. He is considered to have provided the first modern

GOES satellites do visual and infrared imaging of earth atmosphere from [[satellite orbits|geosynchronous orbit]]; they carry secondary payloa

The movement of human-made or natural objects as they enter the atmosphere of a planet from outer space, in the case of Earth from an altitude above t

...late the [[atmospheric reentry]] of a orbital or deep space probe entering atmosphere at especially high speed.

...events are routinely detected by the sensors that are used to monitor the atmosphere for nuclear explosions. June 1908 - [[Tunguska]], [[Russia]]. An object exploded low in the atmosphere, flattening trees over a large area.

Upper portion of a two-part division of the atmosphere (the lower portion is the homosphere) according to the general homogeneity

...h [[combustion]] product gases (''[[flue gas]]es'') are exhausted to the [[atmosphere]]. Includes the draft (draught) effect of hot gases flowing through tall st

The lowest of the main layers of the Earth's atmosphere, extending up about 12km from Earth's surface.

...olor). The artwork is characterized by the search for a vibrant, chromatic atmosphere, bringing them close to the [[impressionism|impressionistic]] tradition.

...mount of heat needed to raise the temperature of 1 gram of water (at one [[Atmosphere (unit)|atm]]) by 1 Celsius. ...lorie'', is measured by heating 1 gram water from 14.5 °C to 15.5 °C at 1 atmosphere absolute pressure. The 4° calorie, also called the ''small calorie'', is m

...e extraction is destructive to the environment, whose burning pollutes the atmosphere, and whose supplies are finite and not renewable.

Layer of the Earth's atmosphere that is directly above the stratosphere and directly below the thermosphere

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* Thomas, G.E. and K. Stamnes (1999). ''Radiative Transfer in the Atmosphere and Ocean'', Cambridge Univiversity Press.

...y]]).<ref>[http://www.srh.noaa.gov/srh/jetstream/atmos/atmos_intro.htm The Atmosphere] From the website of the [[National Oceanic and Atmospheric Administration]

...launching site, for the launch of scientific rockets to explore the upper atmosphere and [[aurora borealis]].

...sub>2</sub>) and [[oxygen]] (O₂) which is the part of [[Earth's atmosphere]] that [[human]]s and all other [[animal]]s breathe in order to obtain the

| [[Liter|L]]·[[atmosphere (unit)|atm]]·K^-1·mol^-1 ==The U.S. Standard Atmosphere's gas constant==

...use gases present in the lower atmosphere. This absorption warms the lower atmosphere.</small> ...he Science of Climate Change</i>, Cambridge Univ. Press.</ref>. The top-of-atmosphere outgoing radiation balances the absorbed 235 W/m² of solar radia

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*[http://telstar.ote.cmu.edu/environ/m3/s2/03earthatmos.shtml Earth & its Atmosphere] From the website of [[Carnegie Mellon University]] Office of Technology fo

| quote=The flow of charged solar particles through the Earth's upper atmosphere is strong enough to ionise atmospheric particles, resulting in the eerie gl When these charged particles interact with the upper atmosphere there are various kinds of exchanges of [[energy]], resulting in the transm

...9_lewin_lec33/ Lecture 33: Kinetic Gas Theory - Ideal Gas Law - Isothermal Atmosphere - Phase Diagrams - Phase Transitions] An excellent, 52 minute video lectur

{{main|Earth's atmosphere|Pressure}} '''Atmospheric pressure''' at any given point in Earth's atmosphere is the downward [[force]] per unit [[area]] exerted upon a horizontal surf

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...9_lewin_lec33/ Lecture 33: Kinetic Gas Theory - Ideal Gas Law - Isothermal Atmosphere - Phase Diagrams - Phase Transitions] An excellent, 52 minute video lectur

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...]]s (62 [[U.S. customary units|miles]]) at a region known as the [[Earth's atmosphere|Kármán line]]. This article is directed less at law, and more at technica {{main|Earth's atmosphere}}

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...of that event with the mother-to-be. Such parties are semi-formal in both atmosphere and content as the environment is one of support and comfort. ...involve like-minded people using virtual interactions to create a festive atmosphere. One example is the [http://en.citizendium.org/wiki/Main_Page Citizendium]

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