Spicule

From Glossary of Meteorology

spicule[edit | edit source]

  1. A spike of ice formed during the freezing of a water drop or a contained volume of water (as in a puddle or freezer container); expansion of the inward freezing ice expels any remaining water through a weak point in the shell which then freezes as a spike in the colder environment.
  2. Rapidly changing, predominantly vertical spike-like structures in the solar chromosphere and observed extending from the solar limb. Spicules appear to be ejected from the low chromosphere at velocities of 20–30 km s−1 and can reach heights of 9000 km before falling back or fading. Their total lifetime generally spans 5–10 minutes.


Term edited 10 September 2018.

Copyright 2024 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact [email protected]. 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.