During the winter of 1997-98, the NASA-Glenn Twin Otter research aircraft completed more than 50 hours of flight in a variety of conditions over the Great Lakes region. Numerous encounters with FZDZ and FZRA are complemented by a large amount of data for conventional icing and no-icing situations. The aircraft was well equipped for sampling and identifying these conditions, and data collected by it provides reliable information for accurately determining the 3-D locations of icing, no-icing, SLD, and no-SLD. In this paper, Twin Otter data are directly compared with IIDA output to examine the algorithm's ability to identify SLD, no-SLD, and no-icing.
This paper provides the first absolute verification of diagnoses or forecasts SLD conditions aloft. The technique applied is fairly strict, as only IIDA output for the adjacent horizontal grid points that were within 1000 feet of the aircraft altitude. For each 3-D grid point, IIDA provides estimates of the potential for icing and SLD. This scaled, rather than binary, icing field allows for an assessment of the ability of the algorithm to discriminate between higher and lower likelihood of icing and SLD. Results are very encouraging. IIDA indicated high or moderate potentials for icing and SLD for most of the Twin Otter icing and SLD encounters, respectively. IIDA also demonstrated capability for differentiating between "yes" and "no" icing and SLD situations.