Small-scale deformation of an Arctic sea ice floe detected by GPS and satellite imagery
Special issue Korean Arctic Ocean Expeditions (K-PORT) in the Northern Chukchi Sea.-- 18 pages, 13 figures, 3 tables Small-scale (~100-200 m) deformations of an Arctic sea ice floe were detected from multiple GPS-equipped buoys that were deployed on the same ice floe. Over a nine-month period three...
| Published in: | Deep Sea Research Part II: Topical Studies in Oceanography |
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| Main Authors: | , , |
| Other Authors: | , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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Pergamon Press
2015
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| Subjects: | |
| Online Access: | http://hdl.handle.net/10261/123948 https://doi.org/10.1016/j.dsr2.2015.01.007 https://doi.org/10.13039/501100000780 https://doi.org/10.13039/501100000782 https://doi.org/10.13039/100000006 https://doi.org/10.13039/501100004837 https://doi.org/10.13039/501100003566 |
| Summary: | Special issue Korean Arctic Ocean Expeditions (K-PORT) in the Northern Chukchi Sea.-- 18 pages, 13 figures, 3 tables Small-scale (~100-200 m) deformations of an Arctic sea ice floe were detected from multiple GPS-equipped buoys that were deployed on the same ice floe. Over a nine-month period three deformation events were recorded. At each case the event was of limited duration, each lasting less than a day. The events were highly compressive in nature with the area occupied by the buoy array decreasing by over half of the original area. The strain rate during the deformation, of the order of 10 -5 s -1 , is about three orders of magnitude larger than previous estimates for brittle fracturing for cracks of about 100m in length. On the 2 day time scale, the strain rate became too small and none of the deformation events could be detected. This suggests that satellite data with longer time scales may significantly underestimate the amount of intermittent, small-scale brittle failure of total deformation. Taken as a whole, our results show the influence that large-scale wind stress can have on small-scale deformation. However, it is important to note that the impact of large-scale wind stress is also dependent on the properties of sea ice as well as on the spatial and temporal evolution of the underlying forces that influence the fracturing process. © 2015 This work was partly supported by ACCESS, an European Project within the Ocean of Tomorrow call of the European Commission Seventh Framework Programme; SATICE, an European Science Foundation (ESF) PolarCLIMATE Programme project; the Marginal Ice Zone (MIZ) Programme by the Office of Naval Research (ONR), United States; the Spanish Ministry of Science and Innovation (MICINN; now MINECO); and the K-PORT (KOPRI, PM13020) Project funded by the Ministry of Oceans and Fisheries (MOF), South Korea. We acknowledge grateful support from Korea Polar Research Institute (KOPRI), South Korea, and the captain and crews of IBRV Araon during the ARA04B cruise. We also thank ... |
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