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Smith Glacier
Improved Estimation of the Mass Balance of Glaciers Draining Into the Amundsen Sea Sector of West Antarctica from the CECS/NASA 2002 Campaign
I!Ij 1)11 U.S
First Exposure Ages from the Amundsen Sea Embayment, West Antarctica: the Late Quaternary Context for Recent Thinning of Pine Island, Smith, and Pope Glaciers
The Last Glaciation of Bear Peninsula, Central Amundsen Sea
Grounding Line Retreat of Pope, Smith, and Kohler Glaciers, West
In This Issue
Widespread, Rapid Grounding Line Retreat of Pine Island, Thwaites, Smith, and Kohler Glaciers, West Antarctica, from 1992 To
Accelerated Glacier Melting in West Antar Melting in West Antarctica
Understanding Antarctic Ice-Stream Flow Using Ice-Flow Models and Geophysical
Article Is Available Online At
Widespread, Rapid Grounding Line Retreat of Pine Island, Thwaites, Smith, and Kohler Glaciers, West Antarctica, from 1992 to 2011
Atmosphere-Ocean-Ice Interactions in the Amundsen Sea Embayment
Reprints from the 1997 Online Issues of Antarctic Journal September Through December
Retreat of Thwaites Glacier, West Antarctica, Over the Next 100 Years Using Various Ice flow Models, Ice Shelf Melt Scenarios and Basal Friction Laws
Aurora Subglacial Basin, East Antarctica Derived by an Ice-Dynamics-Based Interpolation Scheme
Improved Estimation of the Mass Balance of Glaciers Draining Into the Amundsen Sea Sector of West Antarctica from the CECS/NASA 2002 Campaign
Measurement of Ice Flow Velocities from GPS Positions Logged by Short-Period Seismographs in East Antarctica Lei FU1,2,3, Jingxue GUO4 & Xiaofei CHEN1,2,3*
Elevation Changes in Pine Island Glacier, Walgreen Coast, Antarctica, Based on GLAS (2003) and ERS-1 (1995) Altimeter Data Analyses and Glaciological Implications
Top View
Deep Glacial Troughs and Stabilizing Ridges Unveiled Beneath the Margins of the Antarctic Ice Sheet
Weak Bed Control of the Eastern Shear Margin of Thwaites Glacier, West Antarctica
Article Is Available On- Science-Pds.Cryosat.Esa.Int/, Last Access: 31 April 2019
Extensive Dynamic Thinning on the Margins of the Greenland and Antarctic Ice Sheets
Temperate Ice in the Shear Margins of the Antarctic Ice Sheet: Controlling Processes and Preliminary Locations ∗ Colin R
DUNCAN A. YOUNG, Ph. D. Institute for Geophysics • Jackson School Of
A Thermomechanical Model of Ice Flow in West Antarctica
Deep Glacial Troughs and Stabilizing Ridges Unveiled Beneath the Margins of the Antarctic Ice Sheet
Changes in Ice Dynamics and Mass Balance of the Antarctic Ice Sheet