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Glaciers

机译:冰河

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摘要

Its not often that glaciers take centre stage on the covers of the most prestigious general science journals and so it is fitting to start off this review article with reference to two small offerings by glacial researchers to Nature in an issue whose cover is emblazoned with an image of the Matanuska Glacier in Alaska. The scientific breakthrough that merits this high-profile treatment is the discovery of supercooling in overdeepenings at glacier beds, a subject that figures significantly in previous Glaciers reviews in PIPG (Evans, 1999, 2001). The impact of the supercooling process is reviewed by Piotrowski (2003) and then applied by Alley et al. (2003) to a model of stabilizing feedback in the erosion of glacier beds. Examples of possible supercooling are now coming into print thick and fast (e.g., Roberts et al., 2002) but one can not help feeling that glacial researchers can be their own worst enemies by latching on to a newly proposed process–form relationship and promoting it almost to the exclusion of all other equally plausible mechanisms (see Knight, 2003).
机译:冰川并不经常出现在最负盛名的普通科学期刊的封面上,因此,本文以冰川研究人员为《自然》杂志提供的两份小型出版物作为参考,开始这篇评论文章是合适的,该期刊的封面上印有图像。拉斯州马塔努斯卡冰川的全景。值得一提的科学突破是在冰川床的深水层中发现过冷现象,这一点在PIPG先前的冰川评论中得到了重要体现(Evans,1999,2001)。 Piotrowski(2003)回顾了过冷过程的影响,然后由Alley等人应用。 (2003年)的模型在冰川床侵蚀稳定反馈。现在,可能出现过冷的例子越来越多(例如,Roberts等,2002),但人们不禁会以为冰川研究者可能会成为自己最大的敌人,那就是依靠新提出的过程-形式关系并促进它几乎排除了所有其他同样合理的机制(参见Knight,2003年)。

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