Fig. 10: Evaluation of the sensitivity of R and S to the seismometer location in the ice column. | Nature Communications

Fig. 10: Evaluation of the sensitivity of R and S to the seismometer location in the ice column.

From: Observed positive feedback between surface ablation and crevasse formation drives glacier acceleration and potential surge

Fig. 10

(Upper panels) Comparison between the variations of S inferred from the borehole seismometers (location 9—green line and location 4—red line) and the variations of S inferred from the surface seismometers (locations 8 and 3) for the years 2021 (left panel) and 2022 (right panel). (Lower panels) Comparison between R inferred from the borehole seismometers (location 9—green line and location 4—red line) and R inferred from the surface seismometers (locations 8 and 3) for the years 2021 (left panel) and 2022 (right panel). Note that for the year 2021, only data of locations 8 and 9 are available. Note the same range in all y-axis.

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