Results 251 to 260 of about 917,323 (294)
Digital elevation models for the Lambert Glacier–Amery Ice Shelf system, East Antarctica, from ERS-1 satellite radar altimetry [PDF]
, 2000 H. A. Fricker +3 more
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Tidal Modulation of Buoyant Flow and Basal Melt Beneath Petermann Gletscher Ice Shelf, Greenland. [PDF]
J Geophys Res Oceans, 2020 Washam P +3 more
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Seasonal Outflow of Ice Shelf Water Across the Front of the Filchner Ice Shelf, Weddell Sea, Antarctica. [PDF]
Geophys Res Lett, 2018 Darelius E, Sallée JB.
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The Springtime Influence of Natural Tropical Pacific Variability on the Surface Climate of the Ross Ice Shelf, West Antarctica: Implications for Ice Shelf Thinning. [PDF]
Sci Rep, 2018 Clem KR, Orr A, Pope JO.
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Meltwater produced by wind-albedo interaction stored in an East Antarctic ice shelf
, 2017 J. Lenaerts +12 more
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Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell
Nature, 2018Luke Bennetts +2 more
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The far reach of ice-shelf thinning in Antarctica
Nature Climate Change, 2017Ronja Reese +2 more
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Cold Regions Science and Technology, 1982
Abstract A two-dimensional analysis which neglects profile variation in a lateral direction is presented for a floating viscous ice shelf. It applies to plane flow and to unconfined flow which is within short distances of the symmetry line. It is shown that surface variation can, in time, make a significant contribution to the balance, and yet be too
Morland, Leslie, Shoemaker, E.m.
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Abstract A two-dimensional analysis which neglects profile variation in a lateral direction is presented for a floating viscous ice shelf. It applies to plane flow and to unconfined flow which is within short distances of the symmetry line. It is shown that surface variation can, in time, make a significant contribution to the balance, and yet be too
Morland, Leslie, Shoemaker, E.m.
openaire +3 more sources
Science, 1996 Large ice masses such as ice sheets and ice shelves change as the Earth's climate changes, and can serve as indicators of past climate variation. In his Perspective, Fahnestock discusses observations reported by Rott et al. in the same issue, which show the dramatic collapse
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Science, 1979
A hole was drilled through the Ross Ice Shelf 450 kilometers from the barrier. Scientific sampling through this hole revealed a sparse population of crustaceans, fish, and microbial biomass. The seabed consists of mid-Miocene glaciomarine mud. Geothermal heat flow is average.
B. Lyle Hansen, John W. Clough
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A hole was drilled through the Ross Ice Shelf 450 kilometers from the barrier. Scientific sampling through this hole revealed a sparse population of crustaceans, fish, and microbial biomass. The seabed consists of mid-Miocene glaciomarine mud. Geothermal heat flow is average.
B. Lyle Hansen, John W. Clough
openaire +3 more sources