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- W4241363814 abstract "Abstract Ice-stream discharge fluctuations constitute an independent means of forcing unsteady ice-shelf behavior, and their effect must be distinguished from those of oceanic and atmospheric climate to understand ice-shelf change. In addition, ice-stream-generated thickness anomalies may constitute a primary trigger of ice-rise formation in the absence of major sea-level fluctuations. Such triggering may maintain the current ice-rise population that, in turn, contributes to long-term ice-sheet stability. Here, we show that ice-stream-generated fluctuations of an ideal, two-dimensional ice shelf propagate along two characteristic trajectories. One trajectory permits instantaneous transmission of grounding-line velocity changes to all points down-stream. The other trajectory represents slow transmission of grounding-line thickness changes along Lagrangian particle paths." @default.
- W4241363814 created "2022-05-12" @default.
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- W4241363814 date "1988-01-01" @default.
- W4241363814 modified "2023-09-27" @default.
- W4241363814 title "Ice-shelf Response to Ice-stream Discharge Fluctuations: I. Unconfined Ice Tongues" @default.
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- W4241363814 doi "https://doi.org/10.3189/s002214300000914x" @default.
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