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velocity field, since typical roll angles were relatively small. Fig . 1. Topographic maps showing (a) the WRF domains with 30-arc-s topography (m MSL, color filled following scale at bottom), and (b) model topography from the 1.33-km domain (m MSL) centered on the region surrounding Lake Ontario. Sounding sites, the location of the KTYX radar, and geographic features are shown in (b). Following these corrections, an estimated hydrometeor fall speed can be removed to obtain an estimate of the air
velocity field, since typical roll angles were relatively small. Fig . 1. Topographic maps showing (a) the WRF domains with 30-arc-s topography (m MSL, color filled following scale at bottom), and (b) model topography from the 1.33-km domain (m MSL) centered on the region surrounding Lake Ontario. Sounding sites, the location of the KTYX radar, and geographic features are shown in (b). Following these corrections, an estimated hydrometeor fall speed can be removed to obtain an estimate of the air
