Temperature Changes in First Year Arctic Sea Ice During the Decay Process.
Measurements of the seasonal deterioration of landfast, first year sea ice were made in McDougall Sound, Eastern Canadian Arctic, from early May to July 2002. Ice temperatures were obtained from a temperature chain that was frozen into the ice. The uppermost 0.40 m of ice responded to short-term flu...
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ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:12340980 2023-05-15T14:55:11+02:00 Temperature Changes in First Year Arctic Sea Ice During the Decay Process. Johnston, Michelle Timco, Garry 2002-12-02 text https://nrc-publications.canada.ca/eng/view/accepted/?id=02f88ffc-4da0-4c54-89dc-93d6e23a911b https://nrc-publications.canada.ca/eng/view/object/?id=02f88ffc-4da0-4c54-89dc-93d6e23a911b https://nrc-publications.canada.ca/fra/voir/objet/?id=02f88ffc-4da0-4c54-89dc-93d6e23a911b unknown Proceedings of the 16th IAHR International Symposium on Ice, December 2-6, 2002, Volume: 2, Publication date: 2002-12-02, Pages: 194–202 article 2002 ftnrccanada 2021-09-01T06:20:42Z Measurements of the seasonal deterioration of landfast, first year sea ice were made in McDougall Sound, Eastern Canadian Arctic, from early May to July 2002. Ice temperatures were obtained from a temperature chain that was frozen into the ice. The uppermost 0.40 m of ice responded to short-term fluctuations in air temperature. Ice below a depth of 0.50 m showed longer-term response to the steady increase in air temperature. During the decay process, the winter profile of increasing ice temperature with increasing depth reversed; the upper ice surface was warmer than the bottom ice. A systematic increase in ice temperature was observed in ice at all depths. Warming rates decreased linearly from top to bottom, from 0.26°C/day to 0.03°C/day respectively. An analysis showed that the rate of ice decay could be approximated knowing the air temperature/ice surface temperature, ice thickness, and its depth-dependent warming rate. NRC publication: Yes Article in Journal/Newspaper Arctic Sea ice National Research Council Canada: NRC Publications Archive Arctic McDougall Sound ENVELOPE(-97.002,-97.002,75.168,75.168) |
institution |
Open Polar |
collection |
National Research Council Canada: NRC Publications Archive |
op_collection_id |
ftnrccanada |
language |
unknown |
description |
Measurements of the seasonal deterioration of landfast, first year sea ice were made in McDougall Sound, Eastern Canadian Arctic, from early May to July 2002. Ice temperatures were obtained from a temperature chain that was frozen into the ice. The uppermost 0.40 m of ice responded to short-term fluctuations in air temperature. Ice below a depth of 0.50 m showed longer-term response to the steady increase in air temperature. During the decay process, the winter profile of increasing ice temperature with increasing depth reversed; the upper ice surface was warmer than the bottom ice. A systematic increase in ice temperature was observed in ice at all depths. Warming rates decreased linearly from top to bottom, from 0.26°C/day to 0.03°C/day respectively. An analysis showed that the rate of ice decay could be approximated knowing the air temperature/ice surface temperature, ice thickness, and its depth-dependent warming rate. NRC publication: Yes |
format |
Article in Journal/Newspaper |
author |
Johnston, Michelle Timco, Garry |
spellingShingle |
Johnston, Michelle Timco, Garry Temperature Changes in First Year Arctic Sea Ice During the Decay Process. |
author_facet |
Johnston, Michelle Timco, Garry |
author_sort |
Johnston, Michelle |
title |
Temperature Changes in First Year Arctic Sea Ice During the Decay Process. |
title_short |
Temperature Changes in First Year Arctic Sea Ice During the Decay Process. |
title_full |
Temperature Changes in First Year Arctic Sea Ice During the Decay Process. |
title_fullStr |
Temperature Changes in First Year Arctic Sea Ice During the Decay Process. |
title_full_unstemmed |
Temperature Changes in First Year Arctic Sea Ice During the Decay Process. |
title_sort |
temperature changes in first year arctic sea ice during the decay process. |
publishDate |
2002 |
url |
https://nrc-publications.canada.ca/eng/view/accepted/?id=02f88ffc-4da0-4c54-89dc-93d6e23a911b https://nrc-publications.canada.ca/eng/view/object/?id=02f88ffc-4da0-4c54-89dc-93d6e23a911b https://nrc-publications.canada.ca/fra/voir/objet/?id=02f88ffc-4da0-4c54-89dc-93d6e23a911b |
long_lat |
ENVELOPE(-97.002,-97.002,75.168,75.168) |
geographic |
Arctic McDougall Sound |
geographic_facet |
Arctic McDougall Sound |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_relation |
Proceedings of the 16th IAHR International Symposium on Ice, December 2-6, 2002, Volume: 2, Publication date: 2002-12-02, Pages: 194–202 |
_version_ |
1766326961982930944 |