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Snow density along the route traversed by the Japanese-Swedish Antarctic Expedition 2007/08
| Title: | Snow density along the route traversed by the Japanese-Swedish Antarctic Expedition 2007/08 |
| Authors: | Sugiyama, Shin Browse this author →KAKEN DB | | Enomoto, Hiroyuki Browse this author | | Fujita, Shuji Browse this author | | Fukui, Kotaro Browse this author | | Nakazawa, Fumio Browse this author | | Holmlund, Per Browse this author | | Surdyk, Sylviane Browse this author |
| Issue Date: | Jun-2012 |
| Publisher: | International Glaciological Society |
| Journal Title: | Journal of Glaciology |
| Volume: | 58 |
| Issue: | 209 |
| Start Page: | 529 |
| End Page: | 539 |
| Publisher DOI: | 10.3189/2012JoG11J201 |
| Abstract: | During the Japanese-Swedish Antarctic traverse expedition of 2007/08, we measured the surface snow density at 46 locations along the 2800 km long route from Syowa station to Wasa station in East Antarctica. The mean snow density for the upper 1 (or 0.5) m layer varied from 333 to 439 kg m^[-3] over a region spanning an elevation range of 365-3800 m a.s.l. The density variations were associated with the elevation of the sampling sites; the density decreased as the elevation increased, moving from the coastal region inland. However, the density was relatively insensitive to the change in elevation along the ridge on the Antarctic plateau between Dome F and Kohnen stations. Because surface wind is weak in this region, irrespective of elevation, the wind speed was suggested to play a key role in the near-surface densification. The results of multiple regression performed on the density using meteorological variables were significantly improved by the inclusion of wind speed as a predictor. The regression analysis yielded a linear dependence between the density and the wind speed, with a coefficient of 13.5 kg m^[-3] (m s^[-1])^[-1]. This relationship is nearly three times stronger than a value previously computed from a dataset available in Antarctica. Our data indicate that the wind speed is more important to estimates of the surface snow density in Antarctica than has been previously assumed. |
| Rights: | © 2012 International Glaciological Society |
| Relation: | http://www.igsoc.org/ |
| Type: | article |
| URI: | http://hdl.handle.net/2115/50785 |
| 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: 杉山 慎
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