Difference between revisions of "Air"

From Glossary of Meteorology
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== air ==
 
== air ==
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<div class="definition"><div class="short_definition">Mixture of gases forming the earth's [[atmosphere]], consisting of nitrogen (&sim;78 percent), oxygen (&sim;21 percent), [[water vapor]], and other [[trace gas|trace gases]] such as carbon dioxide, helium, argon, [[ozone]], or various pollutants.</div><br/> <div class="paragraph">The concentration of water vapor is very variable, being a strong function of [[temperature]] and, hence, [[altitude]] in the atmosphere. [[dry air|Dry air]] is referred to as air from which measurable amounts of water vapor have been physically removed. Pure, dry air has a [[density]] of 1.293 kg m<sup>-3</sup> at a temperature of 273 K and a [[pressure]] of 101.325 kPa. Apart from the variability of water vapor, the composition of air is essentially constant to an altitude of at least 50 km and is presently approximated as follows.[[File:ams2001glos-At1.gif|link=|center|ams2001glos-At1]]The concentration of ozone is variable, between 10 and 0.1 parts per million. Carbon dioxide, methane, and nitrous oxide have all been increasing since the beginning of the industrial age.</div><br/> </div>
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<div class="definition"><div class="short_definition">Mixture of gases forming Earth's [[atmosphere]], consisting of nitrogen (∼78%), oxygen (∼21%), [[water vapor]], and other [[trace gas|trace gases]] such as carbon dioxide, helium, argon, [[ozone]], or various pollutants.</div><br/>
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<div class="paragraph">The concentration of water vapor is very variable, being a strong function of [[temperature]] and, hence, [[altitude]] in the atmosphere. [[dry air|Dry air]] is referred to as air from which measurable amounts of water vapor have been physically removed. Pure, dry air has a [[density]] of 1.293 kg m<sup>&minus;3</sup> at a temperature of 273 K and a [[pressure]] of 101.325 kPa. Apart from the variability of water vapor, the composition of air is essentially constant to an altitude of at least 50 km and is presently approximated as follows.<br /><br />
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[[File:Air_table_revised.PNG|link=|center|revised air table]]<br />
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The concentration of ozone is variable, between approximately 10 and 0.01 ppm. Carbon dioxide, methane, and nitrous oxide have all been increasing since the beginning of the industrial age. Carbon dioxide and methane concentrations vary by season and location.</div> <br/></div>
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<p>''Term revised 26 June 2017.''</p>
  
 
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Latest revision as of 12:05, 26 June 2017



air

Mixture of gases forming Earth's atmosphere, consisting of nitrogen (∼78%), oxygen (∼21%), water vapor, and other trace gases such as carbon dioxide, helium, argon, ozone, or various pollutants.

The concentration of water vapor is very variable, being a strong function of temperature and, hence, altitude in the atmosphere. Dry air is referred to as air from which measurable amounts of water vapor have been physically removed. Pure, dry air has a density of 1.293 kg m−3 at a temperature of 273 K and a pressure of 101.325 kPa. Apart from the variability of water vapor, the composition of air is essentially constant to an altitude of at least 50 km and is presently approximated as follows.

revised air table

The concentration of ozone is variable, between approximately 10 and 0.01 ppm. Carbon dioxide, methane, and nitrous oxide have all been increasing since the beginning of the industrial age. Carbon dioxide and methane concentrations vary by season and location.

Term revised 26 June 2017.