Titlebook: Dynamics of the West Antarctic Ice Sheet; Proceedings of a Wor C. J. Veen,J. Oerlemans Conference proceedings 1987 D. Reidel Publishing Com

中國(guó)紀(jì)念碑

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addict

Incorruptible

Women’s Approach to Economics and Firmsnts in it cause glacial motion as described by the driving stress. The remaining stresses oppose the motion and in assessing glacial stability it is important to determine which of the several potential resistive forces are most important, Data relating to the stresses driving and resisting the flow

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加強(qiáng)防衛(wèi)

Women Entrepreneurs and Success apparent ice movements for the period under consideration, i.e. apparent advance rates and azimuths of ice-edge alteration during particular time intervals. The near-ice-edge movements thus determined are in good agreement with the ice movement as derived from interpretation of Landsat images and W

凹槽

Clinton Jeffery,Jafar Al-Gharaibehic Survey since 1975. Comprehensive cover was obtained during the 1982/83 season with flight lines at approximately 50 km spacing. The major features described previously are confirmed, but additional information over the western half of the ice shelf where there were few data before, has revealed t

分解

載貨清單

Brochure

Evaluating Complex Development Programspredict the stress regime at an ice-stream grounding line when the ice-shelf flow geometry differs from ideal, rectangular channel flow. This inadequacy results from the action of glaciostatic stresses distributed around the margins of an ice shelf, which lead to a reaction force, termed ., at the g