Archive for June, 2007

“Enhanced-V” and “Warm Trench” IR signatures

Tuesday, June 19th, 2007

AWIPS MODIS IR image

Severe thunderstorms developed over northwestern Kansas on 19 June 2007. An AWIPS image of the MODIS 11.0µm InfraRed (IR) channel (above) revealed an “enhanced-v” and a “warm trench” IR signature on adjacent storm tops. The coldest cloud top brightness temperature values were -77º C on both signatures; the warmest IR temperature associated with the “enhanced-v” was -58º C, while the warmest IR temperature in the “warm trench” was -61º C. You can get a sense that such a “trench” can surround an overshooting top by examining astronaut photography of thunderstorms taken from the space shuttle (image courtesy of Earth Sciences and Image Analysis Laboratory, NASA Johnson Space Center).

AWIPS MODIS IR image

A closer view of the MODIS IR image with a different color enhancement (above) shows that both IR signatures were surrounded by clusters of negative (yellow) and positive (red) cloud-to-ground (CG) lightning strikes. SPC storm reports listed hail (up to 1.75 inches in diameter) within 1 hour of the MODIS image in the region of both IR signatures, but only the southernmost enhanced-v storm produced a tornado; however, higher radar reflectivity values (65-70 dBz) were seen with the northernmost “warm trench” storm.

AWIPS MODIS + GOES IR images

A comparison of the GOES-12 and MODIS IR images (above) demonstrates the better detection capability of these types of IR signatures using 1-km resolution MODIS IR imagery (vs 4-km resolution GOES IR imagery). The IR channels on the next-generation GOES-R Advanced Baseline Imager (ABI) will have a 2-km resolution.

GOES-12 10.7µm IR  image

GOES-12 10.7µm IR imagery (above; 100-image QuickTime animation) showed that these severe thunderstorms in Kansas persisted into the nighttime hours, and eventually became part of a very large Mesoscale Convective Complex (MCC) farther to the south over Oklahoma and Texas. Note the large number of IR pixels exhibiting brightness temperatures of -80º C or colder (violet enhancement) after 02:02 UTC; IR brightness temperatures were as cold as -93º C on a 23:22 UTC NOAA-12 AVHRR IR image, and as cold as -84º C on 05:10/05:13 UTC GOES / MODIS IR images (with 4159 negative and 334 positive CG lightning strikes at that time). Later SPC storm reports included hail up to 4.25 inches in diameter in Kansas (at around 00:05 UTC), and wind gusts to 94 mph in Texas (at around 07:09 UTC).

Severe Convection in Montana

Saturday, June 16th, 2007

GOES-11 10.7µm IR image

Severe thunderstorms developed across parts of Montana on 16 June 2007, producing heavy rainfall (2-6 inches), large hail (up to 3 inches in diameter), damaging winds (gusting to 89 mph), and isolated tornadoes (SPC storm reports). GOES-11 10.7µm InfraRed (IR) imagery (above; Java animation) indicated cloud top brightness temperature values were as cold as -68º C (dark red enhancement) with these storms.

GOES-11 visible image

A closer view using GOES-11 visible channel imagery (above; Java animation) shows the storms in the Billings (KBIL) and Glasgow (KGGW) regions. Of particular interest was the northernmost Glasgow storm, whose northwest-to-southeast track deviated from that of the other eastward or northeastward-moving areas of convection over eastern Montana that day. Also note that the southernmost Billings storm exhibited a well-defined anvil plume after about 00:00 UTC on 17 June — this anvil plume was quite apparent in the visible imagery, but did not seem to exhibit much of a signal in the IR imagery (below).

GOES-11 visible + IR image

The large hail (driven by strong winds) from the northernmost Glasgow storm produced extensive damage to the wheat, alfalfa, and corn crops in that region — Tanja Fransen (WCM, NWS Glasgow) alerted us to the fact that the northwest-to-southeast oriented hail damage swath was clearly evident on Aqua MODIS true color imagery on 20 June, 4 days following the storm (below). A Java image fader applet allows a comparison between the MODIS images on 10 June (before the storm) and 20 June (after the storm), further highlighting hail damage swath. NWS Glasgow measured the damage swath to be about 285 miles long, and up to 12 miles wide (NWS public information statement).

Aqua MODIS true color image