Mechanisms controlling the temporal variation of the sea ice edge in the Southern Ocean
This paper examines the mechanism controlling the short time-scale variation of sea ice cover over the Southern Ocean. Sea ice concentration and ice velocity datasets derived from images of the Defense Meteorological Satellite Program (DMSP) Special Sensor Microwave Imager (SSM/I) are employed to re...
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| Published in | Journal of oceanography Vol. 63; no. 4; pp. 685 - 694 |
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| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
Tokyo
Springer Nature B.V
01.08.2007
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| Subjects | |
| Online Access | Get full text |
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| Abstract | This paper examines the mechanism controlling the short time-scale variation of sea ice cover over the Southern Ocean. Sea ice concentration and ice velocity datasets derived from images of the Defense Meteorological Satellite Program (DMSP) Special Sensor Microwave Imager (SSM/I) are employed to reveal this mechanism. The contribution of both dynamic and thermodynamic processes to the change in ice edge location is examined by comparing the meridional velocity of ice edge displacement and sea ice drift. In the winter expansion phase, the thermodynamic process of new ice production off the ice edge plays an important role in daily advances of ice cover, whereas daily retreats are mostly due to southward ice drift. On the other hand, both advance and retreat of ice edges in the spring contraction phase are mostly caused by the dynamic process of the ice drift. Based on the above mechanism and the linear relation between the degree of ice production at the ice edge and northward wind speed, the seasonal advance of ice cover can be roughly reproduced using the meridional velocity of ice drift at the ice edge.[PUBLICATION ABSTRACT] |
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| AbstractList | This paper examines the mechanism controlling the short time-scale variation of sea ice cover over the Southern Ocean. Sea ice concentration and ice velocity datasets derived from images of the Defense Meteorological Satellite Program (DMSP) Special Sensor Microwave Imager (SSM/I) are employed to reveal this mechanism. The contribution of both dynamic and thermodynamic processes to the change in ice edge location is examined by comparing the meridional velocity of ice edge displacement and sea ice drift. In the winter expansion phase, the thermodynamic process of new ice production off the ice edge plays an important role in daily advances of ice cover, whereas daily retreats are mostly due to southward ice drift. On the other hand, both advance and retreat of ice edges in the spring contraction phase are mostly caused by the dynamic process of the ice drift. Based on the above mechanism and the linear relation between the degree of ice production at the ice edge and northward wind speed, the seasonal advance of ice cover can be roughly reproduced using the meridional velocity of ice drift at the ice edge. This paper examines the mechanism controlling the short time-scale variation of sea ice cover over the Southern Ocean. Sea ice concentration and ice velocity datasets derived from images of the Defense Meteorological Satellite Program (DMSP) Special Sensor Microwave Imager (SSM/I) are employed to reveal this mechanism. The contribution of both dynamic and thermodynamic processes to the change in ice edge location is examined by comparing the meridional velocity of ice edge displacement and sea ice drift. In the winter expansion phase, the thermodynamic process of new ice production off the ice edge plays an important role in daily advances of ice cover, whereas daily retreats are mostly due to southward ice drift. On the other hand, both advance and retreat of ice edges in the spring contraction phase are mostly caused by the dynamic process of the ice drift. Based on the above mechanism and the linear relation between the degree of ice production at the ice edge and northward wind speed, the seasonal advance of ice cover can be roughly reproduced using the meridional velocity of ice drift at the ice edge.[PUBLICATION ABSTRACT] |
| Author | Kimura, Noriaki |
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| CitedBy_id | crossref_primary_10_1002_joc_1933 crossref_primary_10_1007_s10872_022_00669_y crossref_primary_10_1007_s00382_018_4348_3 crossref_primary_10_1371_journal_pone_0064756 crossref_primary_10_1111_j_1600_0870_2011_00526_x crossref_primary_10_2151_sola_2011_005 |
| Cites_doi | 10.1029/90JC02273 10.1029/94JC00707 10.1016/S0034-4257(96)00220-9 10.1029/JC091iC03p03913 10.1029/2000JC000733 10.1029/JD089iD04p05355 10.1175/1520-0493(1982)110<0699:SEITEO>2.0.CO;2 10.2151/jmsj.2004.1223 10.1029/93JC03449 10.1029/94JC01146 10.1029/2000GL011495 10.1029/91JC02333 10.1029/2003JC002235 10.1029/92JC01367 10.1029/2000JC000739 10.1029/JC091iC09p10725 |
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| Title | Mechanisms controlling the temporal variation of the sea ice edge in the Southern Ocean |
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