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Formation processes of sea ice floe size distribution in the interior pack and its relationship to the marginal ice zone off East Antarctica
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| Title: | Formation processes of sea ice floe size distribution in the interior pack and its relationship to the marginal ice zone off East Antarctica |
| Authors: | Toyota, Takenobu Browse this author →KAKEN DB | | Kohout, Alison Browse this author | | Fraser, Alexander D. Browse this author |
| Keywords: | Sea-ice | | Floe size distribution | | Ice melting | | Scale invariance |
| Issue Date: | 24-Oct-2015 |
| Publisher: | Elsevier |
| Journal Title: | Deep Sea Research Part II Topical Studies in Oceanography |
| Volume: | 131 |
| Start Page: | 28 |
| End Page: | 40 |
| Publisher DOI: | 10.1016/j.dsr2.2015.10.003 |
| Abstract: | To understand the behavior of the Seasonal Ice Zone (SIZ), which is composed of sea-ice floes of various sizes, knowledge of the floe size distribution (FSD) is important. In particular, FSD in the Marginal Ice Zone (MIZ), controlled by wave-ice interaction, plays an important role in determining the retreating rates of sea-ice extent on a global scale because the cumulative perimeter of floes enhances melting. To improve the understanding of-wave-ice interaction and subsequent effects on FSD in the MIZ, FSD measurements were conducted off East Antarctica during the second Sea Ice Physics and Ecosystems eXperiment (SIPEX-2) in late winter 2012. Since logistical reasons limited helicopter operations to two interior ice regions, FSD in the interior ice region was determined using a combination of heli-photos and MODIS satellite visible images. The possible effect of wave-ice interaction in the MIZ was examined by comparison with past results obtained in the same MIZ, with our analysis showing: (1) FSD in the interior ice region is basically scale invariant for both small- (< 100 m) and large- (> 1 km) scale regimes; (2) although fractal dimensions are quite different between these two regimes, they are both rather close to that in the MIZ; and (3) for floes < 100 m in diameter, a regime shift which appeared at 20-40 m in the MIZ is absent. These results indicate that one role of wave-ice interaction is to modulate the FSD that already exists in the interior ice region, rather than directly determine it. The possibilities of floe-floe collisions and storm-induced lead formation are considered as, possible formation processes of FSD in the interior pack. (C) 2015 Elsevier Ltd. All rights reserved. |
| Rights: | ©2015, Elsevier. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/ | | http://creativecommons.org/licenses/by-nc-nd/4.0/ |
| Type: | article (author version) |
| URI: | http://hdl.handle.net/2115/67364 |
| Appears in Collections: | 低温科学研究所 (Institute of Low Temperature Science) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)
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Submitter: 豊田 威信
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