首页    期刊浏览 2024年11月30日 星期六
登录注册

文章基本信息

  • 标题:Buoyancy-driven lacustrine calving, Glaciar Nef, Chilean Patagonia
  • 本地全文:下载
  • 作者:Charles Warren ; Doug Benn ; Vanessa Winchester
  • 期刊名称:Journal of Glaciology
  • 印刷版ISSN:0022-1430
  • 电子版ISSN:1727-5652
  • 出版年度:2001
  • 卷号:47
  • 期号:156
  • 页码:135-146
  • DOI:10.3189/172756501781832403
  • 出版社:Cambridge University Press
  • 摘要:Glaciar Nef, a 164 km 2 eastern outlet of Hielo Patagónico Norte (the northern Patagonia icefield), terminates in a proglacial lake that has formed in conjunction with 20th-century glacier retreat. The terminus is inferred to be transiently afloat. A hinge-calving mechanism is proposed in which buoyant forces impose a torque on the glacier tongue, resulting in the release of coherent sections of the glacier tongue as “tabular” icebergs. A simple model shows how torque and tensile stress reach a maximum at the up-glacier limit of the buoyant zone, and that glacier thinning causes this point to migrate up-glacier. Empirical evidence supporting this model includes elevated thermo-erosional notches ≤6.5 m above lake level, and the ubiquitous presence since 1975 of “tabular” icebergs with surface areas ≤0.3 km 2 . Flow speeds of 1.2–1.3 m d −1 were measured near the terminus in February 1998. Extrapolations from these short-term data yield a calving rate of 785–835 m a −1 and a calving flux of 232 × 10 6 m 3 a −1 or 0.2 km 3 a −1 . The calculated mean water depth at the terminus is 190 m. This calving rate is higher than at grounded temperate glaciers calving in fresh water, but is nevertheless almost an order of magnitude less than calving rates at both grounded and floating tidewater glaciers.
国家哲学社会科学文献中心版权所有