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[NORMAL] The impact of weather and climate variability upon estimates of ice-sheet mass balance from satellite radar altimeters

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Figure

Figure 1.1a (left) the apparent change in elevation of the Antarctic ice sheet elevation change was calculated using equation (1.1)
Figure 2.1 The mechanisms responsible for the altimeter echo. The
Figure 2.10 The average of the 400 simulated echoes from the locations shown in
Figure 3.4 Variations in elevation, temperature, accumulation rate and the diameter
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