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Toward autonomous surface-based infrared remote sensing of polar clouds: retrievals of cloud optical and microphysical properties

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Figure

Figure 1. (a) Clear- and cloudy-sky downwelling radiance(1 RU = 1 mW/(m2 sr cm−1)) for a typical polar atmosphere at aresolution of 0.5 cm−1
Table 2. Microwindows used in the optical and microphysical cloudproperty retrievals. The first column gives the central wavenumber,and the second column gives the microwindow width for resolutionsof 0.1 to 4 cm−1
Figure 2. Error contours for retrievals of ice effective radius (rice),ice fraction, and cloud optical depth, as root-mean-square error inradiances for an ice-only cloud
Table 3. Root-mean-square errors in retrieved cloud properties forbase set of spectra due to model error only (no errors imposed) forspectral resolutions indicated
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