Plane-dendritic crystals: Difference between revisions

From Glossary of Meteorology
imported>Perlwikibot
(Redirected page to Plane-dendritic crystal)
 
(CSV import)
 
(One intermediate revision by the same user not shown)
Line 1: Line 1:
 
#REDIRECT [[Plane-dendritic crystal]]
#REDIRECT [[plane-dendritic crystal]]
 
{{TermHeader}}
{{TermSearch}}
 
<div class="termentry">
  <div class="term">
== plane-dendritic crystal ==
  </div>
 
<div class="definition"><div class="short_definition">(''Or'' plane dendrite; sometimes called stellar crystal.) An [[ice crystal]] exhibiting  an elaborately branched (dendritic) structure of hexagonal symmetry, with its much larger  dimension lying perpendicular to the principal (c axis) of the [[crystal]].</div><br/> <div class="paragraph">Such crystals usually form by vapor [[deposition]] at atmospheric temperatures between about  -14&#x000b0; and -18&#x000b0;C. In sufficient concentration they readily aggregate to [[snowflakes]] by interlocking  of their branches. <br/>''See'' [[dendrite]].</div><br/> </div>
</div>
 
{{TermIndex}}
{{TermFooter}}
 
[[Category:Terms_P]]

Latest revision as of 14:07, 11 March 2024

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.