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Albedo-Ice Regression method for determining ice water content of polar mesospheric clouds using ultraviolet observations from space

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Figure

Figure 1. Linear regressions of model PMC albedo versus model PMC ice water content. The black points represent model clouds withreff < 40 nm
Figure 2. Relative errors of ensemble averages,AIR approximation, taken over all cloud model simulations for con-ditions of summer solstice.IWC in the vertical axis, so thatIWC
Figure 4. Illustration showing how IWC = 98 gkm−2 (horizon-tal arrow) and A(90◦) = 16 G (thick downward arrow) are derivedfrom the AIR method from a single measurement of cloud albedo at60 G and SA = 50◦ (upward arrow)
Figure 6. Polar projection map of IWC from CIPS, day 180 (28 June 2012). Panels (a) and (b) show the operational IWC product and theAIR result, respectively.
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