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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3 Jun 2025 - 04:27 EDT
3 Jun 2025 - 08:27 UTC
GOES-19 Full Disk - Tropospheric Dust Content
2 hour loop - 12 images - 10 minute update
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Tropospheric Dust Content - RGB for identifying tropospheric dust - 03 Jun 2025 - 0620 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 03 Jun 2025 - 0630 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 03 Jun 2025 - 0640 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 03 Jun 2025 - 0650 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 03 Jun 2025 - 0700 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 03 Jun 2025 - 0710 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 03 Jun 2025 - 0720 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 03 Jun 2025 - 0730 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 03 Jun 2025 - 0740 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 03 Jun 2025 - 0750 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 03 Jun 2025 - 0800 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 03 Jun 2025 - 0810 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.