Dry-adiabatic process: Difference between revisions

From Glossary of Meteorology
imported>Rbrandt
imported>Rbrandt
 
Line 11: Line 11:
#<div class="definition"><div class="short_definition">An adiabatic process in which no [[condensation]] of its [[water vapor]] occurs and no liquid  water is present.</div><br/>
#<div class="definition"><div class="short_definition">An adiabatic process in which no [[condensation]] of its [[water vapor]] occurs and no liquid  water is present.</div><br/>


<div class="paragraph"><br/>''See'' [[adiabatic process]], [[moist-adiabatic process]].</div><br/>
<div class="paragraph"><br/>''See'' [[adiabatic process]], [[moist-adiabatic process]], [[dry-adiabatic lapse rate]].</div><br/>


<p>''Term edited 20 December 2019.''</p></div><br/>
<p>''Term edited 20 December 2019.''</p></div><br/>

Latest revision as of 12:47, 20 December 2019



dry-adiabatic process

  1. An adiabatic process in a hypothetical atmosphere in which no moisture is present.

  2. An adiabatic process in which no condensation of its water vapor occurs and no liquid water is present.


Term edited 20 December 2019.



Copyright 2024 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact permissions@ametsoc.org. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S.Copyright Act (17 USC § 108) does not require AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, require written permission or a license from AMS. Additional details are provided in the AMS Copyright Policy statement.