Tropospheric ozone: Difference between revisions

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|Meaning=A term used to distinguish [[ozone]] present in the [[troposphere]] from the more  commonly talked about stratospheric [[ozone layer]].
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|Explanation=Tropospheric ozone results from [[transport]] from the [[stratosphere]] and from photochemical  production ([[oxidation]] of [[carbon monoxide]], [[methane]], and other [[hydrocarbons]]). In remote  regions of the troposphere, production and loss of ozone are nearly in balance, while in regions  impacted by [[anthropogenic]] NO<sub>''x''</sub> and hydrocarbon emissions, net ozone production occurs.
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== tropospheric ozone ==
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<div class="definition"><div class="short_definition">A term used to distinguish [[ozone]] present in the [[troposphere]] from the more  commonly talked about stratospheric [[ozone layer]].</div><br/> <div class="paragraph">Tropospheric ozone results from [[transport]] from the [[stratosphere]] and from photochemical  production ([[oxidation]] of [[carbon monoxide]], [[methane]], and other [[hydrocarbons]]). In remote  regions of the troposphere, production and loss of ozone are nearly in balance, while in regions  impacted by [[anthropogenic]] NO<sub>''x''</sub> and hydrocarbon emissions, net ozone production occurs.</div><br/> </div>
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Latest revision as of 01:01, 29 March 2024

A term used to distinguish ozone present in the troposphere from the more commonly talked about stratospheric ozone layer.

Tropospheric ozone results from transport from the stratosphere and from photochemical production (oxidation of carbon monoxide, methane, and other hydrocarbons). In remote regions of the troposphere, production and loss of ozone are nearly in balance, while in regions impacted by anthropogenic NOx and hydrocarbon emissions, net ozone production occurs.

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