Alternating unit tensor: Difference between revisions

From Glossary of Meteorology
imported>Perlwikibot
(Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == alternating unit tensor == </div> <div class="definition"><div class="short_definition">A m...")
m (Rewrite with Template:Term and clean up)
 
(One intermediate revision by the same user not shown)
Line 1: Line 1:
 
{{Term
 
|Display title=alternating unit tensor
{{TermHeader}}
|Definitions={{Definition
{{TermSearch}}
|Num=1
 
|Meaning=A mathematical function with symbol &#x003b5;<sub>''ijk''</sub> defined to switch between the  discrete values of +1, 0, and -1, depending on the values of the three indices ''i'', ''j'', and ''k'':
<div class="termentry">
|Explanation=<blockquote>[[File:ams2001glos-Ae16.gif|link=|center|ams2001glos-Ae16]]</blockquote> It is one of the tools used in [[Einstein's summation notation]] to handle operations equivalent to  cross products in [[vector]] notation. For example: '''A''' &times; '''B''' = &#x003b5;<sub>''ijk''</sub>''A''<sub>''i''</sub>''B''<sub>''j''</sub>&#x003b4;<sub>''k''</sub>, where ''A''<sub>''i''</sub> and ''B''<sub>''j''</sub> represent  vectors in [[summation notation]], and &#x003b4;<sub>''k''</sub> is the unit vector. Subscripts or indices ''i'', ''j'', and ''k'' must  each take on the values of 1, 2, and 3, representing the Cartesian directions of ''x'', ''y'', and ''z''. The  alternating unit tensor is useful to describe the Coriolis term in the [[equations of motion]]: &part;''U''<sub>''i''</sub>/  &part;''t'' = . . . + ''f''&#x003b5;<sub>''ij''3</sub>''U''<sub>''j''</sub> + . . ., where ''f'' is the [[Coriolis parameter]], ''U''<sub>''i''</sub> and ''U''<sub>''j''</sub> are [[wind]] components,  and ''t'' is time. Summation notation is commonly used in [[atmospheric turbulence]] studies.<br/> Stull, R. B. 1988. An Introduction to Boundary Layer Meteorology.  666 pp.  
  <div class="term">
}}
== alternating unit tensor ==
}}
  </div>
 
<div class="definition"><div class="short_definition">A mathematical function with symbol &#x003b5;<sub>''ijk''</sub> defined to switch between the  discrete values of +1, 0, and -1, depending on the values of the three indices ''i'', ''j'', and ''k'':</div><br/> <div class="paragraph"><div class="display-formula"><blockquote>[[File:ams2001glos-Ae16.gif|link=|center|ams2001glos-Ae16]]</blockquote></div> It is one of the tools used in [[Einstein's summation notation]] to handle operations equivalent to  cross products in [[vector]] notation. For example: '''A''' &times; '''B''' = &#x003b5;<sub>''ijk''</sub>''A''<sub>''i''</sub>''B''<sub>''j''</sub>&#x003b4;<sub>''k''</sub>, where ''A''<sub>''i''</sub> and ''B''<sub>''j''</sub> represent  vectors in [[summation notation]], and &#x003b4;<sub>''k''</sub> is the unit vector. Subscripts or indices ''i'', ''j'', and ''k'' must  each take on the values of 1, 2, and 3, representing the Cartesian directions of ''x'', ''y'', and ''z''. The  alternating unit tensor is useful to describe the Coriolis term in the [[equations of motion]]: &part;''U''<sub>''i''</sub>/  &part;''t'' = . . . + ''f''&#x003b5;<sub>''ij''3</sub>''U''<sub>''j''</sub> + . . ., where ''f'' is the [[Coriolis parameter]], ''U''<sub>''i''</sub> and ''U''<sub>''j''</sub> are [[wind]] components,  and ''t'' is time. Summation notation is commonly used in [[atmospheric turbulence]] studies.</div><br/> </div><div class="reference">Stull, R. B. 1988. An Introduction to Boundary Layer Meteorology.  666 pp. </div><br/>
</div>
 
{{TermIndex}}
{{TermFooter}}
 
[[Category:Terms_A]]

Latest revision as of 21:17, 13 January 2024

A mathematical function with symbol εijk defined to switch between the discrete values of +1, 0, and -1, depending on the values of the three indices i, j, and k:
ams2001glos-Ae16
It is one of the tools used in Einstein's summation notation to handle operations equivalent to cross products in vector notation. For example: A × B = εijkAiBjδk, where Ai and Bj represent vectors in summation notation, and δk is the unit vector. Subscripts or indices i, j, and k must each take on the values of 1, 2, and 3, representing the Cartesian directions of x, y, and z. The alternating unit tensor is useful to describe the Coriolis term in the equations of motion: ∂Ui/ ∂t = . . . + fεij3Uj + . . ., where f is the Coriolis parameter, Ui and Uj are wind components, and t is time. Summation notation is commonly used in atmospheric turbulence studies.
Stull, R. B. 1988. An Introduction to Boundary Layer Meteorology. 666 pp.


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.