Optical pathlength: Difference between revisions

From Glossary of Meteorology
(Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == optical pathlength == </div> <div class="definition"><div class="short_definition">(Sometim...")
 
m (Rewrite with Template:Term and clean up)
 
Line 1: Line 1:
 
{{Term
 
|Display title=optical pathlength
{{TermHeader}}
|Definitions={{Definition
{{TermSearch}}
|Num=1
 
|Meaning=(Sometimes called [[optical path]] or optical length.) The [[line integral]] of the  [[refractive index]] (real part) along a [[ray]] connecting two points in an [[optically homogeneous]]  medium.
<div class="termentry">
|Explanation=Because refractive index depends on [[frequency]], so does optical pathlength. Although optical  pathlength may be shortened to optical path, there is a difference between a path and its length.  <br/>''Compare'' [[optical thickness]].
  <div class="term">
}}
== optical pathlength ==
}}
  </div>
 
<div class="definition"><div class="short_definition">(Sometimes called [[optical path]] or optical length.) The [[line integral]] of the  [[refractive index]] (real part) along a [[ray]] connecting two points in an [[optically homogeneous]]  medium.</div><br/> <div class="paragraph">Because refractive index depends on [[frequency]], so does optical pathlength. Although optical  pathlength may be shortened to optical path, there is a difference between a path and its length.  <br/>''Compare'' [[optical thickness]].</div><br/> </div>
</div>
 
{{TermIndex}}
{{TermFooter}}
 
[[Category:Terms_O]]

Latest revision as of 03:27, 27 March 2024

(Sometimes called optical path or optical length.) The line integral of the refractive index (real part) along a ray connecting two points in an optically homogeneous medium.

Because refractive index depends on frequency, so does optical pathlength. Although optical pathlength may be shortened to optical path, there is a difference between a path and its length.
Compare optical thickness.

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.