Flow of water
; Glaciers
; Lakes
; Digital elevation model
; Horizontal flows
; Intermittent-contacts
; Island
; Pine
; Pine island glaciers
; Speckle tracking
; Subglacial waters
; Parallel flow
; bathymetry
; digital elevation model
; displacement
; drainage
; grounding line
; lake
; speckle
; subglacial environment
; subsidence
; TerraSAR-X
; tidal range
; uplift
; water flow
; Antarctica
; Pine Island Glacier
; West Antarctica
Polar Science Center, Applied Physics Lab, University of Washington, Seattle, WA, United States
Recommended Citation:
Joughin I.,Shean D.E.,Smith B.E.,et al. Grounding line variability and subglacial lake drainage on Pine Island Glacier, Antarctica[J]. Geophysical Research Letters,2016-01-01,43(17).