Acoustic tomography: Difference between revisions

From Glossary of Meteorology
imported>Perlwikibot
(Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == acoustic tomography == </div> <div class="definition"><div class="short_definition">An imag...")
m (Rewrite with Template:Term and clean up)
Line 1: Line 1:
 
{{Term
 
|Display title=acoustic tomography
{{TermHeader}}
|Definitions={{Definition
{{TermSearch}}
|Num=1
 
|Meaning=
<div class="termentry">
An imaging technique in which information is collected from beams of acoustic  radiations that have passed through an object, generally in the form representing a two-dimensional  slice through the object.<br/> In [[oceanography]], acoustic tomography consists of an inverse technique that uses acoustic  signals to sample the interior of the ocean. In this way, the [[temperature]] structure of the interior  ocean can be reconstructed from acoustic signals in multiple vertical planes.
  <div class="term">
}}
== acoustic tomography ==
}}
  </div>
 
<div class="definition"><div class="short_definition">An imaging technique in which information is collected from beams of acoustic  radiations that have passed through an object, generally in the form representing a two-dimensional  slice through the object.</div><br/> <div class="paragraph">In [[oceanography]], acoustic tomography consists of an inverse technique that uses acoustic  signals to sample the interior of the ocean. In this way, the [[temperature]] structure of the interior  ocean can be reconstructed from acoustic signals in multiple vertical planes.</div><br/> </div>
</div>
 
{{TermIndex}}
{{TermFooter}}
 
[[Category:Terms_A]]

Revision as of 16:13, 7 November 2023

An imaging technique in which information is collected from beams of acoustic radiations that have passed through an object, generally in the form representing a two-dimensional slice through the object.
In oceanography, acoustic tomography consists of an inverse technique that uses acoustic signals to sample the interior of the ocean. In this way, the temperature structure of the interior ocean can be reconstructed from acoustic signals in multiple vertical planes.


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.