Herzberg continuum: Difference between revisions

From Glossary of Meteorology
(Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == Herzberg continuum == </div> <div class="definition"><div class="short_definition">The port...")
 
m (Rewrite with Template:Term and clean up)
 
(One intermediate revision by the same user not shown)
Line 1: Line 1:
 
{{Term
 
|Display title=Herzberg continuum
{{TermHeader}}
|Definitions={{Definition
{{TermSearch}}
|Num=1
 
|Meaning=The portion of the [[UV]] spectrum of molecular [[oxygen]] (O<sub>2</sub>) between 200 and  240 nm.
<div class="termentry">
|Explanation=The [[absorption]] results from forbidden [[electronic transitions]] from the molecular [[ground state]]  to a number of electronically [[excited states]]. [[photolysis|Photolysis]] of O<sub>2</sub> is dominated by the Herzberg  continuum throughout the [[stratosphere]].
  <div class="term">
}}
== Herzberg continuum ==
}}
  </div>
 
<div class="definition"><div class="short_definition">The portion of the [[UV]] spectrum of molecular [[oxygen]] (O<sub>2</sub>) between 200 and  240 nm.</div><br/> <div class="paragraph">The [[absorption]] results from forbidden [[electronic transitions]] from the molecular [[ground state]]  to a number of electronically [[excited states]]. [[Photolysis]] of O<sub>2</sub> is dominated by the Herzberg  continuum throughout the [[stratosphere]].</div><br/> </div>
</div>
 
{{TermIndex}}
{{TermFooter}}
 
[[Category:Terms_H]]

Latest revision as of 12:54, 30 March 2024

The portion of the UV spectrum of molecular oxygen (O2) between 200 and 240 nm.

The absorption results from forbidden electronic transitions from the molecular ground state to a number of electronically excited states. Photolysis of O2 is dominated by the Herzberg continuum throughout the stratosphere.

Retrieved from "https://glossary.ametsoc.org/w/index.php?title=Herzberg_continuum&oldid=38512"
Powered by MediaWiki
Powered by WikiTeq
Powered by Semantic MediaWiki
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.