GOES-13 6.5 Âµm water vapor imagery + surface fronts
On a rare “High Risk” SPC Convective Outlook day, a significant tornado outbreak occurred across the Deep South region of the US on 24 April 2010 which produced long-track tornadoes that were responsible for at least 10 fatalities across parts of Mississippi (SPC storm reports | NWS Jackson MS event summary). AWIPS images of the GOES-13 6.5 Âµm water vapor channel data with overlays of surface fronts (above) showed a cold frontal boundary advancing eastward across the region, with a strong punch of dry air aloft associated with an upper level jet stream. The NAM model fields suggested that the maximum winds within the jet core were in the 140-145 knot range, but there were a number of MADIS 1-hour interval atmospheric motion vectors with speeds of 155-157 knots along the sharp dry-to-moist water vapor gradient.
Widespread cloudiness obstructed a good view of the amount of Total Precipitable Water (TPW) that was available using the GOES Sounder or MODIS, but the Blended Total Precipitable Water product (below) showed that TPW values of 40 – 50 mm (red to violet color enhancement) were in place within the warm sector ahead of the cold front.
Blended Total Precipitable Water product
An animation of GOES-13 10.7 Âµm IR images (below) revealed that the cluster of severe convection appeared to intensify as it crossed the Mississippi River from Louisiana into Mississippi after about 16 UTC. While there was not the typical “enhanced-v” storm top signature that is often seen with severe convection, the GOES-13 IR cloud top brightness temperatures did cool to -60Âº C and below (darker red color enhancement) after 13:40 UTC, reaching a minimum value of -63Âº C at 18:32 UTC.
Closer views of the IR imagery showed that these storms were characterized by a great deal of cloud to ground lightning strikes (24-hour total lightning strikes) as they produced a number of tornado and damaging wind reports. Farther to the north, there was a report of softball-size hail (4.5 inches in diameter) in western Tennessee at 21:00 UTC.
GOES-13 10.7 Âµm IR images + METAR surface reports
A comparison of a 1-km resolution MODIS 11.0 Âµm IR image with the corresponding 4-km resolution GOES-13 10.7 Âµm IR image as the core of the storm was crossing the Mississippi River around 16:30 UTC (below) demonstrates (1) the improvement in accuracy of storm top brightness temperature detection with higher spatial resolution (-69Âº C with MODIS, versus -58Âº C with GOES), and (2) the “parallax shift” associated with the relatively large geostationary satellite view angle (note that the storm features are shifted a bit to the northwest on the GOES-13 image). The SPC storm reports of tornadoes and damaging winds within the 16:14 – 17:55 UTC time range are also plotted on the two IR images. A similar AVHRR 10.8 Âµm IR image at 18:40 UTC with an overlay of SPC severe reports can be seen here.
MODIS 11.0 Âµm IR and GOES-13 10.7 Âµm IR images (with overlays of severe reports)
===== 25 April Update =====
Comparison of MODIS true color images from 15 April and 25 April 2010
Viewing a comparison of “before” (15 April) and “after” (25 April) 250-meter resolution MODIS true color images (above) and false color images (below), from the SSEC MODIS Today site, the subtle signature of a portion of the tornado damage path can be seen. Viewing the MODIS true color image using Google Earth, the southwest-to-northeast oriented tornado damage path can be seen extending from the eastern half of Yazoo county into the southern portion of Holmes county in Mississippi. The tornado that struck the Yazoo City area has been given a preliminary damage assessment rating of EF4, with a maximum damage path width of 1.75 miles.
Comparison of MODIS false color images from 15 April and 25 April 2010
===== 28 April Update =====
A comparison of 250-meter resolution Aqua MODIS visible Band 1 and Band 2 images from 28 April 2010Â (below) reveals portions of the tornado damage path across parts of Issaquena and Yazoo counties in Mississippi. In areas with a higher density of trees, the tornado damage path appears as a lighter shade of gray on the Band 1 image, and as a darker shade of gray on the Band 2 image.
Portions of the tornado damage path on MODIS visible band 1 and visible band 2 images
â€¢ Weather Underground radar images
â€¢ AccuWeather WeatherMatrix blog post