Canterbury northwester

From Glossary of Meteorology
Revision as of 09:50, 26 March 2024 by WikiTeq (talk | contribs) (Rewrite with Template:Term and clean up)
(diff) ← Older revision | Latest revision (diff) | Newer revision → (diff)
A strong northwest foehn wind descending the New Zealand Alps onto the Canterbury Plains of South Island, New Zealand.

The nor'wester (as it is called locally) is responsible for strong, warm, gusty winds that can damage crops, cause uprooting of trees in forests, damage buildings and other structures, and cause soil loss. Its drying action increases the need for irrigation on the Canterbury Plains. It can occur throughout the year but has highest frequency in spring. It generally occurs immediately prior to the passage of a cold front over the South Island. It is responsible for the highest recorded air temperature in New Zealand (42.4°C at Rangiora on the Canterbury Plains, 7 February 1973).
McKendry, I. G. 1983. Spatial and temporal aspects of the surface wind regime on the Canterbury Plains, New Zealand. J. Climate. 3. 155–166.
Sturman, A., and N. Tapper 1996. The Weather and Climate of New Zealand. Oxford University Press, . 476 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.