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.
27 Sep 2023 - 18:41 EDT
27 Sep 2023 - 22:41 UTC
GOES-East CONUS - Tropospheric Dust Content
1 hour loop - 12 images - 5 minute update
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Tropospheric Dust Content - RGB for identifying tropospheric dust - 27 Sep 2023 - 2136 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 27 Sep 2023 - 2141 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 27 Sep 2023 - 2146 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 27 Sep 2023 - 2151 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 27 Sep 2023 - 2156 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 27 Sep 2023 - 2201 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 27 Sep 2023 - 2206 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 27 Sep 2023 - 2211 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 27 Sep 2023 - 2216 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 27 Sep 2023 - 2221 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 27 Sep 2023 - 2226 UTC
Tropospheric Dust Content - RGB for identifying tropospheric dust - 27 Sep 2023 - 2231 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.