Results 101 to 110 of about 401,804 (204)
A Method for Rapid Determination of the Icing Limit of a Body in Terms of the Stream Conditions [PDF]
The effects of existing frictional heating were analyzed to determine the conditions under which ice formations on aircraft surfaces can be prevented.
Callaghan, Edmund E., Serafini, John S.
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Ice-Shelf Response to Ice-stream Discharge Fluctuations: III. The Effects of Ice-stream Imbalance on the Ross Ice Shelf, Antarctica [PDF]
Journal of Glaciology, 1989 AbstractA numerical simulation of the Ross Ice Shelf, Antarctica, in which discharge from Ice Streams A-E is changed suddenly between extreme states, is used to investigate ice-shelf thickness and flow anomalies generated by ice-stream transience.
openaire +2 more sources
Geologos, 2015 In the Polish Lowlands, three main ice lobes, referred to as Odra, Vistula and Mazury, formed during the Last Scandinavian Glaciation. These lobes protruded at least several kilometres beyond the main ice margin and it is believed that they represent ...
Hermanowski Piotr
doaj +1 more source
Can Relict Crevasse Plumes on Antarctic Ice Shelves Reveal a History of Ice-Stream Fluctuation? [PDF]
, 1988 Douglas R. MacAyeal +3 more
openalex +1 more source
Numerical simulation of ice growth on a MS-317 swept wing geometry [PDF]
An effort to develop a 3-D ice accretion modeling method was initiated. This first step towards creation of a complete aircraft icing simulation code builds on previously developed methods for calculating 3-D flow fields and particle trajectories ...
Bidwell, C. S., Potapczuk, M. G.
core +1 more source
A Modeling Experiment on the Grounding of an Ice Shelf in the Central Arctic Ocean During MIS 6 [PDF]
, 2003 High-resolution chirp sonar subbottom profiles from the Lomonosov Ridge in the central Arctic Ocean, acquired from the Swedish icebreaker Oden in 1996, revealed large-scale erosion of the ridge crest down to depths of 1000 m below present sea level ...
Jakobsson, Martin +2 more
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Geophysical Research Letters, 2019 Ice streams are bounded by abrupt transitions in speed called shear margins. Some shear margins are fixed by subglacial topography, but others are thought to be selfâorganizing, evolving by thermal feedback to ice viscosity and basal drag which govern ...
N. Holschuh +2 more
doaj +1 more source
Fast glacier flow: Ice streams, surging, and tidewater glaciers [PDF]
, 1987 Garry K. C. Clarke
openalex +1 more source
Ice-Thickness Map of the West Antarctic Ice Streams by Radar Sounding [PDF]
, 1988 Sion Shabtaie, Charles R. Bentley
openalex +1 more source
Ice-Shelf Flexure and Tidal Forcing of Bindschadler Ice Stream, West Antarctica [PDF]
Viscoelastic models of ice-shelf flexure and ice-stream velocity perturbations are combined into a single efficient flowline model to study tidal forcing of grounded ice.
Alley, Richard B. +4 more
core +1 more source