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Cirrus cloud optical and microphysical property retrievals from eMAS during SEAC 4RS using bi-spectral reflectance measurements within the 1.88 µm water vapor absorption band

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Figure

Figure 1. Spectral two-way transmittance (gray line), from TOAto surface, calculated with LBLRTM using a tropical ocean atmo-sphere
Figure 3. Two-channel plot illustrating the sensitivity of the 1.83and 1.93 µm eMAS channels to cloud optical thickness (near-vertical lines) and effective particle radius (near-horizontal lines),respectively.
Figure 4. eMAS CTH, COT, and CER retrievals for a portion of track 8 of the 18 September 2013 SEAC4RS science flight
Figure 5. A comparison of nadir-view ice-phase COTretrievals correspond to the top of each panel in Fig
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