Crater Creek Fire in British Columbia produces a pyrocumulonimbus cloud
![](https://cimss.ssec.wisc.edu/satellite-blog/images/2023/08/bc_4p-20230817_014226.png)
GOES-18 “Red” Visible (0.64 µm) + Fire Power derived product (top left), Shortwave Infrared (3.9 µm, top right), “Clean” Infrared Window (10.3 µm, bottom left) and Cloud Top Temperature derived product (bottom right) [click to play animated GIF | MP4]
![](https://cimss.ssec.wisc.edu/satellite-blog/images/2023/08/230817_0142utc_BC_pyroCb_cursor_sample.png)
Cursor sampling of GOES-18 “Red” Visible (0.64 µm) + Fire Power derived product (top left), Shortwave Infrared (3.9 µm, top right), “Clean” Infrared Window (10.3 µm, bottom left) and Cloud Top Temperature derived product (bottom right) at 0142 UTC [click to enlarge]
![](https://cimss.ssec.wisc.edu/satellite-blog/images/2023/08/230817_0157utc_BC_pyroCb_cursor_sample.png)
Cursor sampling of GOES-18 “Red” Visible (0.64 µm) + Fire Power derived product (top left), Shortwave Infrared (3.9 µm, top right), “Clean” Infrared Window (10.3 µm, bottom left) and Cloud Top Temperature derived product (bottom right) at 0157 UTC [click to enlarge]