Evidence of liquid dependent ice nucleation in high-latitude stratiform clouds from surface remote sensors
Ground-based lidar, radar and microwave radiometer observations at Eureka, Canada, Barrow, Alaska and over the western Arctic Ocean measure physical characteristics and morphology of stratiform clouds. Despite transition of a cold atmosphere (−15 C)through ice supersaturated conditions, ice is not o...
Published in: | Geophysical Research Letters |
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Format: | Article in Journal/Newspaper |
Language: | English |
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American Geophysical Union
2011
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Online Access: | http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-512 https://doi.org/10.1029/2010GL046016 |
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ftncar:oai:drupal-site.org:articles_10762 2023-09-05T13:17:18+02:00 Evidence of liquid dependent ice nucleation in high-latitude stratiform clouds from surface remote sensors de Boer, G. (author) Morrison, Hugh (author) Shupe, M. (author) Hildner, R. (author) 2011-01-06 application/pdf http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-512 https://doi.org/10.1029/2010GL046016 en eng American Geophysical Union Geophysical Research Letters http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-512 doi:10.1029/2010GL046016 wos: 000286061200004 ark:/85065/d7280852 An edited version of this paper was published by AGU. Copyright 2011 American Geophysical Union. Text article 2011 ftncar https://doi.org/10.1029/2010GL046016 2023-08-14T18:40:05Z Ground-based lidar, radar and microwave radiometer observations at Eureka, Canada, Barrow, Alaska and over the western Arctic Ocean measure physical characteristics and morphology of stratiform clouds. Despite transition of a cold atmosphere (−15 C)through ice supersaturated conditions, ice is not observed until soon after a liquid layer. Several cases illustrating this phenomenon are presented in addition to long-term observations from three measurement sites characterizing cloud phase frequency. This analysis demonstrates that clouds composed entirely of ice occur less frequently than liquid-topped mixed-phase clouds at temperatures warmer than −25 to −30 C. These results indicate ice formation generally occurs in conjunction with liquid at these temperatures, and suggest the importance of liquid-dependent ice nucleation mechanisms. Article in Journal/Newspaper Arctic Arctic Ocean Barrow Alaska OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Arctic Arctic Ocean Canada Eureka ENVELOPE(-85.940,-85.940,79.990,79.990) Geophysical Research Letters 38 1 n/a n/a |
institution |
Open Polar |
collection |
OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) |
op_collection_id |
ftncar |
language |
English |
description |
Ground-based lidar, radar and microwave radiometer observations at Eureka, Canada, Barrow, Alaska and over the western Arctic Ocean measure physical characteristics and morphology of stratiform clouds. Despite transition of a cold atmosphere (−15 C)through ice supersaturated conditions, ice is not observed until soon after a liquid layer. Several cases illustrating this phenomenon are presented in addition to long-term observations from three measurement sites characterizing cloud phase frequency. This analysis demonstrates that clouds composed entirely of ice occur less frequently than liquid-topped mixed-phase clouds at temperatures warmer than −25 to −30 C. These results indicate ice formation generally occurs in conjunction with liquid at these temperatures, and suggest the importance of liquid-dependent ice nucleation mechanisms. |
author2 |
de Boer, G. (author) Morrison, Hugh (author) Shupe, M. (author) Hildner, R. (author) |
format |
Article in Journal/Newspaper |
title |
Evidence of liquid dependent ice nucleation in high-latitude stratiform clouds from surface remote sensors |
spellingShingle |
Evidence of liquid dependent ice nucleation in high-latitude stratiform clouds from surface remote sensors |
title_short |
Evidence of liquid dependent ice nucleation in high-latitude stratiform clouds from surface remote sensors |
title_full |
Evidence of liquid dependent ice nucleation in high-latitude stratiform clouds from surface remote sensors |
title_fullStr |
Evidence of liquid dependent ice nucleation in high-latitude stratiform clouds from surface remote sensors |
title_full_unstemmed |
Evidence of liquid dependent ice nucleation in high-latitude stratiform clouds from surface remote sensors |
title_sort |
evidence of liquid dependent ice nucleation in high-latitude stratiform clouds from surface remote sensors |
publisher |
American Geophysical Union |
publishDate |
2011 |
url |
http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-512 https://doi.org/10.1029/2010GL046016 |
long_lat |
ENVELOPE(-85.940,-85.940,79.990,79.990) |
geographic |
Arctic Arctic Ocean Canada Eureka |
geographic_facet |
Arctic Arctic Ocean Canada Eureka |
genre |
Arctic Arctic Ocean Barrow Alaska |
genre_facet |
Arctic Arctic Ocean Barrow Alaska |
op_relation |
Geophysical Research Letters http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-512 doi:10.1029/2010GL046016 wos: 000286061200004 ark:/85065/d7280852 |
op_rights |
An edited version of this paper was published by AGU. Copyright 2011 American Geophysical Union. |
op_doi |
https://doi.org/10.1029/2010GL046016 |
container_title |
Geophysical Research Letters |
container_volume |
38 |
container_issue |
1 |
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n/a |
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n/a |
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1776198521739804672 |