On 04 September 2017 a pyroCb formed in British Columbia. GOES-15 detected the smoke plumes and pyroCb cloud, as well as the fires hot spot. The pyroCb cloud (~50.2º N, 115.1ºW) formed around 1:00 UTC . Starting at 0:00 UTC on 04 September, the animation below shows GOES-15 0.63 µm visible (left) and 3.9 µm shortwave IR (right) . In the shortwave IR images, the red pixels indicate very hot IR brightness temperatures exhibited by the fire source regions.
![GOES-15 0.63 µm visible channel (left) and 3.9 µm shortwave IR channel images (right) (click to play animation)](http://pyrocb.ssec.wisc.edu/wp-content/uploads/2017/09/170904_g15_vis2_anim-1024x768.gif)
GOES-15 0.63 µm visible channel (left) and 3.9 µm shortwave IR channel images (right) (click to play animation)
Usually GOES-15 10.7 μm IR channel is used to find the cloud-top IR brightness temperature. However, the resolution of this satellite did not provide a brightness temperature lower than -40ºC.
A 1-km resolution NOAA-19 AVHRR 10.8 µm Infrared Window image (below;courtesy ofRené Servranckx) revealed a minimum cloud-top IR brightness temperature of -53.6º C (red color enhancement) for the pyroCb at 1:12 UTC on 04 September.
![NOAA-19 AVHRR 0.64 µm visible (top left), 3.7 µm shortwave IR (top right), 10.8 µm IR window (bottom left) and false-color RGB composite image (bottom right)](http://pyrocb.ssec.wisc.edu/wp-content/uploads/2017/09/thumbnail_20170904_0112UTC_N18_LAC_ch1_ch3_ch4_ch321.jpg)
NOAA-19 AVHRR 0.64 µm visible (top left), 3.7 µm shortwave IR (top right), 10.8 µm IR window (bottom left) and false-color RGB composite image (bottom right)