Lidar equation: Difference between revisions

From Glossary of Meteorology
(Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == lidar equation == </div> <div class="definition"><div class="short_definition">An equation,...")
 
m (Rewrite with Template:Term and clean up)
 
(One intermediate revision by the same user not shown)
Line 1: Line 1:
 
{{Term
 
|Display title=lidar equation
{{TermHeader}}
|Definitions={{Definition
{{TermSearch}}
|Num=1
 
|Meaning=An equation, which may appear in different forms depending on the particular system  or application, that describes the relation between the [[received power]] ''p'' measured in a [[lidar]]  receiver channel from range ''r'', and the characteristics of the lidar system and the transmission  medium (usually the [[atmosphere]]) through which the [[laser]] pulse propagates.
<div class="termentry">
|Explanation=The most common form of the equation is for plane-polarized [[radiation]] and [[single-scattering|single scattering]],  for which  <blockquote>[[File:ams2001glos-Le15.gif|link=|center|ams2001glos-Le15]]</blockquote> where &beta; is the volume backscattering coefficient at range ''r,'' ''t''<sup>2</sup> is the two-way [[transmittance]] to  range ''r,'' and ''C'' is the [[lidar constant]], which depends on such system parameters as the [[transmitted power|transmitted  power]], [[pulse duration]], and [[receiver]] characteristics. The transmittance is related to the [[volume extinction coefficient|volume  extinction coefficient]] &gamma; by  <blockquote>[[File:ams2001glos-Le16.gif|link=|center|ams2001glos-Le16]]</blockquote> Normally [[scattering]] and [[extinction]] of the lidar beam are caused by the combined effects of  molecules, [[aerosols]], and [[hydrometeors]], so that &beta; and &gamma; represent the sum of their separate  contributions. <br/>''Compare'' [[radar equation]].
  <div class="term">
}}
== lidar equation ==
}}
  </div>
 
<div class="definition"><div class="short_definition">An equation, which may appear in different forms depending on the particular system  or application, that describes the relation between the [[received power]] ''p'' measured in a [[lidar]]  receiver channel from range ''r'', and the characteristics of the lidar system and the transmission  medium (usually the [[atmosphere]]) through which the [[laser]] pulse propagates.</div><br/> <div class="paragraph">The most common form of the equation is for plane-polarized [[radiation]] and [[single scattering]],  for which  <div class="display-formula"><blockquote>[[File:ams2001glos-Le15.gif|link=|center|ams2001glos-Le15]]</blockquote></div> where &beta; is the volume backscattering coefficient at range ''r,'' ''t''<sup>2</sup> is the two-way [[transmittance]] to  range ''r,'' and ''C'' is the [[lidar constant]], which depends on such system parameters as the [[transmitted  power]], [[pulse duration]], and [[receiver]] characteristics. The transmittance is related to the [[volume  extinction coefficient]] &gamma; by  <div class="display-formula"><blockquote>[[File:ams2001glos-Le16.gif|link=|center|ams2001glos-Le16]]</blockquote></div> Normally [[scattering]] and [[extinction]] of the lidar beam are caused by the combined effects of  molecules, [[aerosols]], and [[hydrometeors]], so that &beta; and &gamma; represent the sum of their separate  contributions. <br/>''Compare'' [[radar equation]].</div><br/> </div>
</div>
 
{{TermIndex}}
{{TermFooter}}
 
[[Category:Terms_L]]

Latest revision as of 06:39, 29 March 2024

An equation, which may appear in different forms depending on the particular system or application, that describes the relation between the received power p measured in a lidar receiver channel from range r, and the characteristics of the lidar system and the transmission medium (usually the atmosphere) through which the laser pulse propagates.
The most common form of the equation is for plane-polarized radiation and single scattering, for which
ams2001glos-Le15
where β is the volume backscattering coefficient at range r, t2 is the two-way transmittance to range r, and C is the lidar constant, which depends on such system parameters as the transmitted power, pulse duration, and receiver characteristics. The transmittance is related to the volume extinction coefficient γ by
ams2001glos-Le16
Normally scattering and extinction of the lidar beam are caused by the combined effects of molecules, aerosols, and hydrometeors, so that β and γ represent the sum of their separate contributions.
Compare radar equation.
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.