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A path towards uncertainty assignment in an operational cloud-phase algorithm from ARM vertically pointing active sensors

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Figure

Fig. 1, and the spectra measurements in Fig. 2.To include some of this additional information, a secondmore recent ARM radar data processing methodology, Mi-
Table 1. Time, height, and temperature thresholds defining data used to train the model.
Figure 4. Profiles of(c)lines indata between snow and mixed phase, as well as indicating the regiondepolarization ratios for (a) ice water fraction from aircraft, HSRL (b) the time of the in situ measurements and for a longer period of time
Figure 8. As in Fig. 5, but for 4 October 2004. White outlined areashows liquid cloud.
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