Wind shear: Difference between revisions

From Glossary of Meteorology
imported>Perlwikibot
(Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == wind shear == </div> <div class="definition"><div class="short_definition">The local [[vari...")
 
imported>Perlwikibot
No edit summary
 
Line 9: Line 9:
   </div>
   </div>


<div class="definition"><div class="short_definition">The local [[variation]] of the [[wind vector]] or any of its components in a given direction.</div><br/> <div class="paragraph">The vertical [[shear]] can be expressed in terms of height &part;''V''/&part;''z'' or of [[pressure]] &part;''V''/&part;''p'' as the  vertical coordinate. If the [[wind]] is [[geostrophic]], the vertical shear is given by the [[thermal wind  equation]]. The wind shear at a point is said to be [[cyclonic]] or [[anticyclonic]] according to whether  the sense of rotation from the wind vector to the [[shear vector]] at that point is cyclonic or  anticyclonic.</div><br/> </div>
<div class="definition"><div class="short_definition">The local [[variation]] of the [[wind vector]] or any of its components in a given direction.</div><br/> <div class="paragraph">The vertical [[shear]] can be expressed in terms of height &part;''V''/&part;''z'' or of [[pressure]] &part;''V''/&part;''p'' as the  vertical coordinate. If the [[wind]] is [[geostrophic]], the vertical shear is given by the [[thermal wind equation|thermal wind  equation]]. The wind shear at a point is said to be [[cyclonic]] or [[anticyclonic]] according to whether  the sense of rotation from the wind vector to the [[shear vector]] at that point is cyclonic or  anticyclonic.</div><br/> </div>
</div>
</div>



Latest revision as of 17:16, 25 April 2012



wind shear[edit | edit source]

The local variation of the wind vector or any of its components in a given direction.

The vertical shear can be expressed in terms of height ∂V/∂z or of pressureV/∂p as the vertical coordinate. If the wind is geostrophic, the vertical shear is given by the thermal wind equation. The wind shear at a point is said to be cyclonic or anticyclonic according to whether the sense of rotation from the wind vector to the shear vector at that point is cyclonic or anticyclonic.


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.