Notice:
This site has successfully transitioned the image data source from GOES-16 to
GOES-19. There are some remaining anomalies in the production of mesoscale
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as expected. Please contact:
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30 Apr 2025 - 20:14 EDT
1 May 2025 - 00:14 UTC
GOES-19 CONUS - Tropospheric Dust Content
1 hour loop - 12 images - 5 minute update
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Tropospheric Dust Content - RGB for identifying tropospheric dust - 30 Apr 2025 - 2311 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 30 Apr 2025 - 2316 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 30 Apr 2025 - 2321 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 30 Apr 2025 - 2326 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 30 Apr 2025 - 2331 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 30 Apr 2025 - 2336 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 30 Apr 2025 - 2341 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 30 Apr 2025 - 2346 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 30 Apr 2025 - 2351 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 30 Apr 2025 - 2356 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 01 May 2025 - 0001 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 01 May 2025 - 0006 UTC
Dust RGB key:
1 - Dust plume, day (bright magenta, pink) Note: Dust at night becomes purple shades below 3 km
2 - Low, water cloud (light purple)
3 - Desert surface, day (light blue)
4 - Mid, thick clouds (tan shades)
5 - Mid, thin cloud (green)
6 - Cold, thick clouds (red)
7 - High, thin ice clouds (black)
8 - Very thin clouds, over warm surface (blue)
Dust RGB Dust can be hard to see in visible and infrared imagery because it is optically thin, or because it appears similar to other cloud types such as cirrus. The RGB product is able to contrast airborne dust from clouds using band differencing and the IR thermal channel. The IR band differencing allows dust storms to be observed during both daytime and at night.