GOES-18 Interleave Testing - Has ended. GOES-West data now supplied from operational GOES-17 satellite.
GOES-18 expected to become operational GOES-West in January 2023. See GOES-18 Interleave Testing for more information.
3 Feb 2023 - 18:55 EST
3 Feb 2023 - 23:55 UTC
GOES-West Full Disk - Fire Temperature
2 hour loop - 12 images - 10 minute update
To enlarge, pause animation & click the image. Hover over popups to zoom. Use slider to navigate.
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MS Edge are all supported.
Fire Temperature - RGB used to highlight fires - 03 Feb 2023 - 2140 UTC
Fire Temperature - RGB used to highlight fires - 03 Feb 2023 - 2150 UTC
Fire Temperature - RGB used to highlight fires - 03 Feb 2023 - 2200 UTC
Fire Temperature - RGB used to highlight fires - 03 Feb 2023 - 2210 UTC
Fire Temperature - RGB used to highlight fires - 03 Feb 2023 - 2220 UTC
Fire Temperature - RGB used to highlight fires - 03 Feb 2023 - 2230 UTC
Fire Temperature - RGB used to highlight fires - 03 Feb 2023 - 2240 UTC
Fire Temperature - RGB used to highlight fires - 03 Feb 2023 - 2250 UTC
Fire Temperature - RGB used to highlight fires - 03 Feb 2023 - 2300 UTC
Fire Temperature - RGB used to highlight fires - 03 Feb 2023 - 2310 UTC
Fire Temperature - RGB used to highlight fires - 03 Feb 2023 - 2320 UTC
Fire Temperature - RGB used to highlight fires - 03 Feb 2023 - 2330 UTC
Fire Temperature key:
1 - Warm fire 2 - Very warm fire 3 - Hot fire 4 - Very hot fire 5 - Burn scars 6 - Clear sky: land 7 - Clear sky: water/snow/night 8 - Water clouds 9 - Ice clouds
Fire Temperature RGB allows the user to identify where the most intense fires are occurring and differentiate these from "cooler" fires. The RGB takes advantage of the fact that from 3.9µm to shorter wavelengths, background solar radiation and surface reflectance increases. This means that fires need to be more intense in order to be detected by the 2.2 and 1.6µm bands, as more intense fires emit more radiation at these wavelengths. Therefore, small/"cool" fires will only show up at 3.9µm and appear red while increases in fire intensity cause greater contributions of the other channels resulting in white very intense fires.
