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Okreek Fire in south-central South Dakota

Strong southerly winds (gusting as high as 50 mph) helped a large grassland fire (named the Okreek fire) spread rapidly northward across south-central South Dakota during the afternoon hours on 05 October 2011. The light gray smoke plume and the dark burn scar... Read More

GOES-11 + GOES-15 + GOES-13 visible channel images

GOES-11 + GOES-15 + GOES-13 visible channel images

Strong southerly winds (gusting as high as 50 mph) helped a large grassland fire (named the Okreek fire) spread rapidly northward across south-central South Dakota during the afternoon hours on 05 October 2011. The light gray smoke plume and the dark burn scar grew very quickly, which could be seen on GOES-11 (GOES-West),  GOES-15, and GOES-13 (GOES-East) visible channel images (above). Each of the 3 sets of images is displayed in the native projection of the respective satellite.

The corresponding 3.9 µm shortwave IR images from each satellite (below) showed the large and intense “hot spot” (dark black to yellow pixels) associated with the Okreek fire. Note there were also a few other smaller fires burning in other parts of central South Dakota during that time period, which also exhibited very intense hot spot signatures.

GOES-11 + GOES-15 + GOES-13 shortwave IR images

GOES-11 + GOES-15 + GOES-13 shortwave IR images

A comparison of 250-meter resolution false-color Red/Green/Blue (RGB) images from the SSEC MODIS Today site from before (04 October), during (05 October), and after (07 October) the Okreek fire revealed the development and growth of the 26 mile long burn scar (which appears as the light brown line). The bright pink feature on the 05 October image was the heat signature of the active front line of the fire, which was rapidly advancing northward on that day.

MODIS false-color RGB images from 04 October, 05 October, and 07 October 2011

MODIS false-color RGB images from 04 October, 05 October, and 07 October 2011

 

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Fog and stratus in the Ohio River Valley and central Appalachians

Strong nocturnal radiational cooling beneath a large area of high pressure centered over the Ohio River Valley led to the formation of widespread areas of fog and stratus on 05 October 2011. AWIPS image... Read More

MODIS and GOES-13 fog/stratus product images

MODIS and GOES-13 fog/stratus product images

Strong nocturnal radiational cooling beneath a large area of high pressure centered over the Ohio River Valley led to the formation of widespread areas of fog and stratus on 05 October 2011. AWIPS image comparisons of the 1-km resolution MODIS and the 4-km resolution GOES-13 fog/stratus products at 03:30 UTC or 11:30 pm local time (above) and 07:45 UTC  or 3:45 am local time (below) demonstrated the clear advantage of having improved spatial resolution to detect the more subtle features such as river valley fog.

MODIS and GOES-13 fog/stratus product images

MODIS and GOES-13 fog/stratus product images

 

To compliment the improved fog/stratus detection capabilities offered by higher spatial resolution, other products are being developed (as part of the CIMSS participation in GOES-R Proving Ground activities) that provide more quantitative information about areas of fog and/or low cloud: for example, Fog Depth, Marginal Visual Flight Rules (MVFR) Probability, and Instrument Flight Rules (IFR) Probability (below). In this case, the 07:45 UTC products indicated that the Fog Depth values were as high as 1231 feet (cyan color enhancement) over parts of northern West Virginia, where there were also MVFR Probabilities greater than 90% and IFR Probabilities greater than 75% (brighter red color enhancement).

GOES-13 fog/stratus product, Fog Depth, MVFR Probability, and IFR Probability

GOES-13 fog/stratus product, Fog Depth, MVFR Probability, and IFR Probability

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Sediment features in southern Lake Michigan

As was highlighted in news stories posted by the National Weather Service forecast offices at Chicago and Milwaukee, a large amount of sediment was seen in southern Lake Michigan following a strong wind event which produced very large waves. A... Read More

MODIS true color images: 02 October (left) and 03 October (right)

MODIS true color images: 02 October (left) and 03 October (right)

As was highlighted in news stories posted by the National Weather Service forecast offices at Chicago and Milwaukee, a large amount of sediment was seen in southern Lake Michigan following a strong wind event which produced very large waves. A comparison of 250-meter resolution MODIS true color Red/Green/Blue (RGB) images from the SSEC MODIS Today site (above) showed one particularly large sediment feature protruding northward from the southeastern part of Lake Michigan on 02 October and 03 October 2011.

A comparison of AWIPS images of 1-km resolution MODIS 0.65 µm visible channel data with the corresponding 1-km resolution MODIS Sea Surface Temperature (SST) product on 03 October (below) showed that while the prominent sediment feature was embedded within a larger scale area of warmer waters (SST values in the lower 60s F, darker red color enhancement) in the far southern part of the lake, there was not necessarily a 1:1 correspondence between the sediment pattern and the sea surface temperature pattern.

MODIS 0.65 µm visible channel image + MODIS Sea Surface Temperature product

MODIS 0.65 µm visible channel image + MODIS Sea Surface Temperature product

GOES-13 0.63 µm visible channel imagery (below; click image to play animation) indicated that the prominent sediment feature was moving slowly northward early in the day on 03 October — however, once the northwesterly winds reported by the mid-lake buoy began to increase and gust to 16 knots later in the day, the northward motion of the sediment feature appeared to slow somewhat.

GOES-13 0.63 µm visible channel images (click image to play animation)

GOES-13 0.63 µm visible channel images (click image to play animation)

===== 06 October Update =====

A sequence of daily 250-meter resolution MODIS true color RGB images from 02, 03, 04, 05, and 06 October (below) show the changes in shape and location of the large sediment feature in the southeastern part of Lake Michigan.

MODIS true color images from 02, 03, 04, 05, and 06 October

MODIS true color images from 02, 03, 04, 05, and 06 October

In addition, daily 15-minute interval GOES-15 0.63 µm visible channel images from that same period (below; click image to play 5-day animation) further show how the sediment patterns were transported and morphed by the Lake Michigan water currents.

GOES-15 0.63 µm visible channel images (click image to play 5-day animation)

GOES-15 0.63 µm visible channel images (click image to play 5-day animation)

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Chemical plant fire near Dallas, Texas

A McIDAS image comparison of GOES-11 (GOES-West) 0.65 µm visible channel, GOES-15 0.63 µm visible channel, and GOES-13 (GOES-East) 0.63 µm visible channel data (above) showed the dark smoke plume from a fire burning at a chemical plant in Waxahachie, Texas (about 30 miles south of Dallas) on Read More

GOES-11, GOES-15, and GOES-13 visible channel images

GOES-11, GOES-15, and GOES-13 visible channel images

A McIDAS image comparison of GOES-11 (GOES-West) 0.65 µm visible channel, GOES-15 0.63 µm visible channel, and GOES-13 (GOES-East) 0.63 µm visible channel data (above) showed the dark smoke plume from a fire burning at a chemical plant in Waxahachie, Texas (about 30 miles south of Dallas) on 03 October 2011. (Note: GOES-15 is scheduled to replace GOES-11 as the operational GOES-West satellite in December 2011).

A similar comparison of the GOES-11, GOES-15, and GOES-13 3.9 µm shortwave IR channels (below) indicated that no obvious fire “hot spot” was evident before the appearance of the dark smoke plume — the brighter yellow colors highlight pixels which have an IR brightness temperature hotter than 45º C. This 45º C threshold was exceeded at 16:30 UTC on the GOES-15 and GOES-13 images, and at 16:45 on the GOES-11 images; on the visible channel imagery, the dark smoke plume was seen 30 minutes earlier at 16:00 UTC on all 3 satellites.

GOES-11, GOES-15, and GOES-13 shortwave IR images

GOES-11, GOES-15, and GOES-13 shortwave IR images

A 17:32 UTC Terra MODIS Red/Green/Blue (RGB) true color image from the SSEC MODIS Today site (below, viewed using Google Earth) confirmed the very dark nature of the smoke plume from this particular fire, which was causing some evacuations (news media story).

MODIS true color RGB image (viewed using Google Earth)

MODIS true color RGB image (viewed using Google Earth)

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