Tropical Storm Lee
McIDAS images of 4-km resolution GOES-15 10.7 Âµm IR data (above; click image to play animation) showed the transition of Tropical Depression #13 into Tropical Storm Lee in the northern Gulf of Mexico on 02 September 2011. Deep convection persisted within the eastern semi-circle of the system, with large areas exhibiting cloud top IR brightness temperatures of -80Âº C and colder (violet color enhancement) prior to Lee reaching tropical storm intensity.
A comparison of AWIPS images of 1-km resolution POES AVHRR 0.63 Âµm visible channel and 10.8 Âµm IR channel data (below) revealed a few vigorous overshooting tops embedded within the convective region, with one feature located southeast of the circulation center having an IR brightness temperature value of -93Âº C (darker violet color enhancement).
About 2 hours later, a similar comparison of 1-km resolution MODIS 0.65 Âµm visible channel and 11.0 Âµm IR channel images (below) showed overshooting tops with IR brightness temperatures as cold as -89Âº C.
===== 03 SEPTEMBER UPDATE =====
GOES-13 0.63 Âµm visible channel images (above; click image to play animation; also available as a QuickTime movie) revealed a curious “dual-vortex” structure to Tropical Storm Lee early in the day on 03 September 2011, with convective bursts developing in the vicinity of each of the two vortices. Later in the day, it appears that these dual vortices merged into a single vortex, as the center of Lee approachd the coast of Louisiana.
A comparison of 1-km resolution MODIS 6.7 Âµm and 4-km resolution GOES-13 6.5 Âµm water vapor images (below) showed that a significant tongue of dry continental air was being drawn into the western portion of the circulation of Lee.