In this study, high-level cloud classified by the simple technique using the split window was compared with cloud height observed by Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP). High-level clouds including thin cirrus and cumulonimbus type clouds mostly correspond to the clouds signal higher than 8km by CALIOP observations. High-level cloud classified by the split window also reasonably agreed with the ice phase or mixed phase identified by the use of the 8.7 micron channel of SEVIRI.
The advantage of CALIOP observation is effective in identifying the multi-layer cloud. Double layer cirrus cloud observed by CALIOP corresponded to smaller brightness temperature (TBB) difference between the split window (BTD=TBB11-TBB12) than that of single layer cirrus type cloud. A simple double layer case was simulated by radiation code of RSTAR. It indicates smaller BTD, which corresponds to N-type cloud in the split window cloud type classification method (Inoue, 1987). Some of the N-type cloud by the split window was suggested as multi layer cloud from both CALIOP observations and simulation.
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