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Fig. 2


Example ATPM fits to the (1620) Geographos thermal-infared observations (data points; Green 1985; Veeder et al. 1989; Tedesco et al. 2004) using the radar (dashed lines), flattened-radar (dotted lines), and light-curve (solid lines) shape models. The thermal-infrared spectrum of the flattened-radar shape model in the lower right panel is almost identical to that of the light-curve shape model.

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