1-minute Mesoscale Domain Sector GOES-16 (GOES-East) “Red” Visible (0.64 µm), Shortwave Infrared (3.9 µm), “Clean” Infrared Window (10.35 µm) and Fire Temperature Red-Green-Blue (RGB) images (above) showed a period of extreme behavior of the East Troublesome Fire in Colorado around and just after sunset on 21 October 2020. This rapidly-growing wildfire produced a series of pyrocumulonimbus (pyroCb) clouds — the coldest pyroCb cloud-top 10.35 µm infrared brightness temperatures were -65.1ºC (darker green enhancement). The hottest Shortwave Infrared brightness temperatures within the fire’s large thermal anomaly were 138.7ºC — which is the saturation temperature of 3.9 µm detectors on the ABI instrument of GOES-16.

=====22 October Update =====

A time-matched comparison of Shortwave Infrared images from Suomi NPP VIIRS (3.74 µm) and GOES-16 ABI (3.9 µm), valid at 0839 UTC on 22 October, is shown below. The finer spatial resolution of VIIRS (375 meters at nadir, vs 2 km for ABI) provided a more accurate depiction of the location of hottest fire pixels at that time. Note the amount of northwestward parallax shift of the cold (dark blue to violet) high clouds on the GOES-16 image.

During the subsequent daytime hours, GOES-16 Visible, Shortwave Infrared, Infrared Window and Fire Temperature RGB images (below)  showed another series of pyroCb clouds that were produced by the East Troublesome Fire — but not to the extent that was seen on 21 October. By early evening, the total burned area had increased to 170,163 acres (and was only 5% contained).

Two high-resolution views of some of the pyroCb clouds and the fire’s thermal anomaly were provided by VIIRS Visible (0.64 µm), Shortwave Infrared (3.74 µm) and Infrared Window (11.45 µm) images from NOAA-20 at 1904 UTC and Suomi NPP at 1956 UTC (below).

Additional satellite imagery of this fire event is available on the Satellite Liaison Blog.

===== 23 October Update =====

GOES-16 True Color RGB images created using Geo2Grid (above) revealed the light brown hue associated with smoke from the East Troublesome Fire, which was being transported eastward across the North Atlantic Ocean; the large cloud field of Hurricane Epsilon could also be seen southwest of the smoke pall. The bulk of this smoke pall was being transported along a cold frontal boundary (below).