Handout (973.4 kB)
This study utilizes an extensive observational dataset composed primarily of land-based NEXRAD WSR-88D and airborne NOAA WP-3D Doppler radar data and then supplemented with surface (both onshore and offshore), rawindsondes, GPS dropsondes, and aircraft flight-level data from Hurricanes Ivan and Jeanne of 2004. The three-dimensional wind fields of deep convective cells within offshore hurricane rainbands are documented via dual-Doppler analyses. The thermodynamic structure is inferred from flight-level, GPS dropwindsonde, and surface (buoy) observations. Several cells exhibit supercell characteristics (i.e., rotating updrafts and hook echoes) offshore and two produced tornadoes soon after moving onshore. The same cells, viewed from the land-based WSR-88D radars, exhibit higher echo tops (ETs), greater vertically integrated liquid (VIL), greater rotational shears, and higher spectral widths than nontornadic cells while still offshore. A synopsis of these preliminary (and additional) results will be presented at the conference.
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