A pseudohumidity variable RH' is defined, equal to relative humidity when RH<100% and linearly related to cloud liquid water density when clouds exist. (Saturation is assumed over the entire scene in this case.) An iterative retrieval of RH' is performed using the Jacobian with respect to RH'. A plane parallel, non-precipitating liquid or mixed-phase cloud is assumed with an upper limit of 0.5 mm of cloud liquid water. Scattering is neglected; the presence of precipitation will generally cause the retrieval to fail due to high TB error.
Retrievals were performed using observations simulated from a database of ECMWF analysis temperature, humidity, and cloud profiles. The cloud profiles were adjusted to be plane parallel by removing layers of low cloud fraction and assuming that the remaining layers had 100% cloud cover. Simulated retrievals are able to reproduce cloud top, bottom, and liquid water amount much of the time, with cloud top being slightly underestimated, cloud base slightly overestimated, and total cloud liquid water somewhat underestimated on average. Parameters retrieved from AMSU-B observations are mapped and compared with geostationary infrared images and the output of a visible/infrared-based cloud-classification algorithm.
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