Role of tides in Arctic ocean/ice climate
Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 112 (2007): C04S06, doi:10.1029/2006JC003643. A three-dimensio...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/3589 2023-05-15T14:34:29+02:00 Role of tides in Arctic ocean/ice climate Holloway, Greg Proshutinsky, Andrey 2007-03-28 application/pdf https://hdl.handle.net/1912/3589 en_US eng American Geophysical Union https://doi.org/10.1029/2006JC003643 Journal of Geophysical Research 112 (2007): C04S06 https://hdl.handle.net/1912/3589 doi:10.1029/2006JC003643 Journal of Geophysical Research 112 (2007): C04S06 doi:10.1029/2006JC003643 Tide Arctic Climate Article 2007 ftwhoas https://doi.org/10.1029/2006JC003643 2022-05-28T22:58:00Z Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 112 (2007): C04S06, doi:10.1029/2006JC003643. A three-dimensional coupled ocean/ice model, intended for long-term Arctic climate studies, is extended to include tidal effects. From saved output of an Arctic tides model, we introduce parameterizations for (1) enhanced ocean mixing associated with tides and (2) the role of tides fracturing and mobilizing sea ice. Results show tides enhancing loss of heat from Atlantic waters. The impact of tides on sea ice is more subtle as thinning due to enhanced ocean heat flux competes with net ice growth during rapid openings and closings of tidal leads. Present model results are compared with an ensemble of nine models under the Arctic Ocean Model Intercomparison Project (AOMIP). Among results from AOMIP is a tendency for models to accumulate excessive Arctic Ocean heat throughout the intercomparison period 1950 to 2000 which is contrary to observations. Tidally induced ventilation of ocean heat reduces this discrepancy. This research is supported by the National Science Foundation Office of Polar Programs under cooperative agreements OPP-0002239 and OPP-0327664 with the International Arctic Research Center, University of Alaska Fairbanks. Article in Journal/Newspaper Arctic Arctic Ocean International Arctic Research Center National Science Foundation Office of Polar Programs Sea ice Alaska Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Arctic Arctic Ocean Fairbanks Journal of Geophysical Research 112 C4 |
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Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
topic |
Tide Arctic Climate |
spellingShingle |
Tide Arctic Climate Holloway, Greg Proshutinsky, Andrey Role of tides in Arctic ocean/ice climate |
topic_facet |
Tide Arctic Climate |
description |
Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 112 (2007): C04S06, doi:10.1029/2006JC003643. A three-dimensional coupled ocean/ice model, intended for long-term Arctic climate studies, is extended to include tidal effects. From saved output of an Arctic tides model, we introduce parameterizations for (1) enhanced ocean mixing associated with tides and (2) the role of tides fracturing and mobilizing sea ice. Results show tides enhancing loss of heat from Atlantic waters. The impact of tides on sea ice is more subtle as thinning due to enhanced ocean heat flux competes with net ice growth during rapid openings and closings of tidal leads. Present model results are compared with an ensemble of nine models under the Arctic Ocean Model Intercomparison Project (AOMIP). Among results from AOMIP is a tendency for models to accumulate excessive Arctic Ocean heat throughout the intercomparison period 1950 to 2000 which is contrary to observations. Tidally induced ventilation of ocean heat reduces this discrepancy. This research is supported by the National Science Foundation Office of Polar Programs under cooperative agreements OPP-0002239 and OPP-0327664 with the International Arctic Research Center, University of Alaska Fairbanks. |
format |
Article in Journal/Newspaper |
author |
Holloway, Greg Proshutinsky, Andrey |
author_facet |
Holloway, Greg Proshutinsky, Andrey |
author_sort |
Holloway, Greg |
title |
Role of tides in Arctic ocean/ice climate |
title_short |
Role of tides in Arctic ocean/ice climate |
title_full |
Role of tides in Arctic ocean/ice climate |
title_fullStr |
Role of tides in Arctic ocean/ice climate |
title_full_unstemmed |
Role of tides in Arctic ocean/ice climate |
title_sort |
role of tides in arctic ocean/ice climate |
publisher |
American Geophysical Union |
publishDate |
2007 |
url |
https://hdl.handle.net/1912/3589 |
geographic |
Arctic Arctic Ocean Fairbanks |
geographic_facet |
Arctic Arctic Ocean Fairbanks |
genre |
Arctic Arctic Ocean International Arctic Research Center National Science Foundation Office of Polar Programs Sea ice Alaska |
genre_facet |
Arctic Arctic Ocean International Arctic Research Center National Science Foundation Office of Polar Programs Sea ice Alaska |
op_source |
Journal of Geophysical Research 112 (2007): C04S06 doi:10.1029/2006JC003643 |
op_relation |
https://doi.org/10.1029/2006JC003643 Journal of Geophysical Research 112 (2007): C04S06 https://hdl.handle.net/1912/3589 doi:10.1029/2006JC003643 |
op_doi |
https://doi.org/10.1029/2006JC003643 |
container_title |
Journal of Geophysical Research |
container_volume |
112 |
container_issue |
C4 |
_version_ |
1766307500575948800 |