Noctilucent Clouds Seen from North America

Noctilucent clouds are tenuous ice clouds that form in the upper mesosphere over arctic and subarctic regions in the summer. Observations of the clouds made during 1988 and 1989 by the North American surveillance network NLC CAN AM are presented. Observing took place from 15 May to 15 August, except...

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Published in:ARCTIC
Main Authors: Lohvinenko, Todd W., Zalcik, Mark S.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1991
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64609
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/64609 2023-05-15T14:19:12+02:00 Noctilucent Clouds Seen from North America Lohvinenko, Todd W. Zalcik, Mark S. 1991-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64609 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64609/48523 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64609 ARCTIC; Vol. 44 No. 4 (1991): December: 267–373; 328-336 1923-1245 0004-0843 Noctilucent clouds Alaska Canada Canadian Arctic North America info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1991 ftunivcalgaryojs 2022-03-22T21:21:48Z Noctilucent clouds are tenuous ice clouds that form in the upper mesosphere over arctic and subarctic regions in the summer. Observations of the clouds made during 1988 and 1989 by the North American surveillance network NLC CAN AM are presented. Observing took place from 15 May to 15 August, except for arctic sites, which observed from 1 April to 30 April and 15 August to 15 September due to the Midnight Sun. The peak incidence of noctilucent clouds occurred in July during both years. Both positive and negative sightings, that latter determined by at least two readings under favourable conditions, are plotted on date-latitude graphs. An apparent northern migration of noctilucent clouds (NCL) with latitude as the season progresses was detected. Although an attempt was made to look for an apparent longitudinal drift, none was found. A detailed comparison of how NLC have behaved and changed in the past quarter century is examined using the NCL CAN AM data in conjunction with the 1964-65 data presented by Fogle (1966).Key words: noctilucent clouds, northem migration, longitudinal drift, comparison Mots clés: nuages noctulescents, déplacement vers le nord, dérive en longitude, comparaison Article in Journal/Newspaper Arctic Arctic Subarctic Alaska midnight sun University of Calgary Journal Hosting Arctic Canada ARCTIC 44 4
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Noctilucent clouds
Alaska
Canada
Canadian Arctic
North America
spellingShingle Noctilucent clouds
Alaska
Canada
Canadian Arctic
North America
Lohvinenko, Todd W.
Zalcik, Mark S.
Noctilucent Clouds Seen from North America
topic_facet Noctilucent clouds
Alaska
Canada
Canadian Arctic
North America
description Noctilucent clouds are tenuous ice clouds that form in the upper mesosphere over arctic and subarctic regions in the summer. Observations of the clouds made during 1988 and 1989 by the North American surveillance network NLC CAN AM are presented. Observing took place from 15 May to 15 August, except for arctic sites, which observed from 1 April to 30 April and 15 August to 15 September due to the Midnight Sun. The peak incidence of noctilucent clouds occurred in July during both years. Both positive and negative sightings, that latter determined by at least two readings under favourable conditions, are plotted on date-latitude graphs. An apparent northern migration of noctilucent clouds (NCL) with latitude as the season progresses was detected. Although an attempt was made to look for an apparent longitudinal drift, none was found. A detailed comparison of how NLC have behaved and changed in the past quarter century is examined using the NCL CAN AM data in conjunction with the 1964-65 data presented by Fogle (1966).Key words: noctilucent clouds, northem migration, longitudinal drift, comparison Mots clés: nuages noctulescents, déplacement vers le nord, dérive en longitude, comparaison
format Article in Journal/Newspaper
author Lohvinenko, Todd W.
Zalcik, Mark S.
author_facet Lohvinenko, Todd W.
Zalcik, Mark S.
author_sort Lohvinenko, Todd W.
title Noctilucent Clouds Seen from North America
title_short Noctilucent Clouds Seen from North America
title_full Noctilucent Clouds Seen from North America
title_fullStr Noctilucent Clouds Seen from North America
title_full_unstemmed Noctilucent Clouds Seen from North America
title_sort noctilucent clouds seen from north america
publisher The Arctic Institute of North America
publishDate 1991
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64609
geographic Arctic
Canada
geographic_facet Arctic
Canada
genre Arctic
Arctic
Subarctic
Alaska
midnight sun
genre_facet Arctic
Arctic
Subarctic
Alaska
midnight sun
op_source ARCTIC; Vol. 44 No. 4 (1991): December: 267–373; 328-336
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64609/48523
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64609
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