Homosphere: Difference between revisions
From Glossary of Meteorology
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<div class="definition"><div class="short_definition">The lower portion of a two-part division of the [[atmosphere]] according to the general homogeneity of atmospheric composition; opposed to the [[heterosphere]].</div><br/> <div class="paragraph">The homosphere is the region in which there is no gross change in atmospheric composition, that is, all of the atmosphere from the earth's surface to about 80 or 100 km. <br/>''See'' [[atmospheric shell]].</div><br/> </div> | <div class="definition"><div class="short_definition">The lower portion of a two-part division of the [[atmosphere]] according to the general homogeneity of atmospheric composition; opposed to the [[heterosphere]].</div><br/> <div class="paragraph">The homosphere is the region in which there is no gross change in atmospheric composition, that is, all of the atmosphere from the earth's surface to about 80 or 100 km. <br/>''See'' [[atmospheric shell|atmospheric shell]].</div><br/> </div> | ||
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Latest revision as of 16:09, 25 April 2012
homosphere[edit | edit source]
The lower portion of a two-part division of the atmosphere according to the general homogeneity of atmospheric composition; opposed to the heterosphere.
The homosphere is the region in which there is no gross change in atmospheric composition, that is, all of the atmosphere from the earth's surface to about 80 or 100 km.
See atmospheric shell.
See atmospheric shell.
