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

前面

Affable

Unconfined Ice-Shelf Flow,ss in both directions. Exploiting the slow variation of physical quantities in both horizontal directions compared to vertical variation allows simple solution of the vertical momentum balance and the derivation of plane stress equilibrium equations for integrals of the horizontal stresses through t

正常

小步舞

Ice-Shelf Backpressure: Form Drag Versus Dynamic Drag,predict 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

含糊其辞

Ice Stream-Ice Shelf Interaction in West Antarctica, of base camps which were established in the mouths of ice streams B and C and at the upstream edge of Crary Ice Rise. The annual rate of ice deformation in Ice Stream C is very small, generally less than 10. yr.. Reoccupation of an 11 year old stake network permitted ice motion (6.1 m/yr) and groun

毗邻

键琴

Exclaim

endocardium

A Subglacial Aquifer Bed Model and Water Pressure Dependent Basal Sliding Relationship for a West Age is 3 to 18 m./s at the grounding line. The inferred subglacial water pressure is greater than 90 % of the ice overburden pressure for the entire 300 km length of the ice stream, and greater than 96 % of the ice overburden pressure for 230 km upglacier from the grounding line. This suggests that t

影响

The Heat Budget of the Ross Drainage Basin,s from the fact that dissipative heating can be calculated directly from the release of gravitational energy. When mass balance, surface temperature and geothermal input are known, the mean ice temperature at the grounding line can be obtained as a residual..The procedure is applied to the drainage