Results 81 to 90 of about 401,804 (204)

Ice streams—fast, and faster?

open access: yesComptes Rendus. Physique, 2004
Abstract Rapid flow of ice streams is caused either by great thickness, or by effective basal lubrication especially from deforming tills. Competing thermal processes act to stabilize and to destabilize the well-lubricated ice streams, and may contribute to their observed short-term variability yet long-term persistence. Increasing evidence indicates
Richard B. Alley   +3 more
openaire   +2 more sources

Ice-stream stability on a reverse bed slope [PDF]

open access: yesNature Geoscience, 2012
Marine ice streams whose beds deepen inland are thought to be inherently unstable. Numerical modelling of the Maguerite Bay ice-stream retreat in West Antarctica since the Last Glacial Maximum suggests that an ice stream can stabilize on an inland-sloping bed owing to increased lateral drag where the ice stream narrows.
Jamieson, Stewart S.R.   +6 more
openaire   +5 more sources

First description of subglacial megalineations from the late Paleozoic ice age in southern Africa.

open access: yesPLoS ONE, 2019
We identify late Paleozoic ice age (LPIA) subglacial megalineations from field and geospatial imagery of the Twyfelfontein area of northern Namibia, and present the results of a geomorphometric analysis of those data.
Graham D Andrews   +3 more
doaj   +1 more source

Analysis of Ice Plains of Filchner/Ronne Ice Shelf Using ICESat Data [PDF]

open access: yes, 2010
We use repeat-track laser altimeter data from the Ice, Cloud, and land Elevation Satellite (ICESat) to map the grounding zone of Filchner/Ronne Ice Shelf (FRIS), Antarctica. Repeated passes of ICESat reveal ice flexure in the grounding zone occurs as the
Brunt, Kelly M.   +2 more
core   +1 more source

The impact of temperature and crystal orientation fabric on the dynamics of mountain glaciers and ice streams

open access: yesJournal of Glaciology, 2020
Streaming ice accounts for a major fraction of global ice flux, yet we cannot yet fully explain the dominant controls on its kinematics. In this contribution, we use an anisotropic full-Stokes thermomechanical flow solver to characterize how mechanical ...
Kate Hruby   +5 more
doaj   +1 more source

Analytical analysis of small-amplitude perturbations in the shallow ice stream approximation

open access: yes, 2008
International audienceNew analytical solutions describing the effects of small-amplitude perturbations in boundary data on flow in the shallow ice stream approximation are presented.
Gudmundsson, G. H.
core   +1 more source

Technical note: formation of airborne ice crystals in a wall independent reactor (WIR) under atmospheric conditions [PDF]

open access: yes, 2008
Both, gas and particle scavenging contribute to the transport of organic compounds by ice crystals in the troposphere. To simulate these processes an experimental setup was developed to form airborne ice crystals under atmospheric conditions. Experiments
Fries, Elke   +6 more
core  

The marginal shear stress of Ice Stream B, West Antarctica [PDF]

open access: yes, 1997
To ascertain whether the velocity of Ice Stream B, West Antarctica, may be controlled by the stress in its marginal shear zones (the "Snake" and the "Dragon"), we undertook a determination of the marginal shear stress in the Dragon near Camp Up B by ...
Jackson, Miriam, Kamb, Barclay
core   +1 more source

Left High and Dry: Deglaciation of Dogger Bank, North Sea, Recorded in Proglacial Lake Evolution

open access: yesFrontiers in Earth Science, 2019
Reconstructions of palaeo-ice sheet retreat in response to climate warming using offshore archives can provide vital analogs for future ice-sheet behavior.
Andy R. Emery   +5 more
doaj   +1 more source

Data requirements in support of the marine weather service program [PDF]

open access: yes, 1972
Data support activities for the Marine Weather Service Program are outlined. Forecasts, cover anomolous water levels, including sea and swell, surface and breakers, and storm surge.
Mccaslin, R. W., Mull, M., Travers, J.
core   +1 more source

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