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- W1997835561 abstract "[1] We have used Interferometric Synthetic Aperture Radar (InSAR) data and sequential Landsat imagery to identify and temporally constrain two acceleration events on Pine Island Glacier (PIG). These two events are separated by a period of at least seven years (1987–1994). The change in discharge between two flux gates indicates that the majority of the increase in discharge associated with the second acceleration originates well inland (>80 km) from the grounding line. An analysis indicates that changes in driving stress consistent with observed thinning rates are sufficient in magnitude to explain much of the acceleration." @default.
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- W1997835561 date "2003-07-01" @default.
- W1997835561 modified "2023-10-01" @default.
- W1997835561 title "Timing of Recent Accelerations of Pine Island Glacier, Antarctica" @default.
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- W1997835561 doi "https://doi.org/10.1029/2003gl017609" @default.
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