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
geocolor images which are being investigated. Everything else should be operating
as expected. Please contact:
NESDIS.STAR.webmaster@noaa.gov if you have any questions.
10 Apr 2025 - 10:39 EDT
10 Apr 2025 - 14:39 UTC
GOES-19 Full Disk - Air Mass
2 hour loop - 12 images - 10 minute update
To enlarge, pause animation & click the image. Hover over popups to zoom. Use slider to navigate.
While GOES animation code will not run on older Internet Explorer browsers,
they work in the newest versions of Microsoft Edge. If you are using
Internet Explorer, please try a different browser: Chrome, Firefox, Safari, or
MS Edge are all supported.
Air Mass - RGB based on data from IR & water vapor - 10 Apr 2025 - 1210 UTC
Air Mass - RGB based on data from IR & water vapor - 10 Apr 2025 - 1220 UTC
Air Mass - RGB based on data from IR & water vapor - 10 Apr 2025 - 1230 UTC
Air Mass - RGB based on data from IR & water vapor - 10 Apr 2025 - 1240 UTC
Air Mass - RGB based on data from IR & water vapor - 10 Apr 2025 - 1300 UTC
Air Mass - RGB based on data from IR & water vapor - 10 Apr 2025 - 1310 UTC
Air Mass - RGB based on data from IR & water vapor - 10 Apr 2025 - 1320 UTC
Air Mass - RGB based on data from IR & water vapor - 10 Apr 2025 - 1330 UTC
Air Mass - RGB based on data from IR & water vapor - 10 Apr 2025 - 1340 UTC
Air Mass - RGB based on data from IR & water vapor - 10 Apr 2025 - 1400 UTC
Air Mass - RGB based on data from IR & water vapor - 10 Apr 2025 - 1410 UTC
Air Mass - RGB based on data from IR & water vapor - 10 Apr 2025 - 1420 UTC
Key for AirMass RGB:
1 - Jet stream / potential vorticity (PV) / deformation zones / dry upper level (dark red / orange)
2 - Cold air mass (dark blue/purple)
3 - Warm air mass (green)
4 - Warm air mass, less moisture (olive/dark orange)
5 - High thick cloud (white)
6 - Mid level cloud (tan/salmon)
7 - Low level cloud (green, dark blue)
8 - Limb effects (purple/blue)
Air Mass RGB is used to diagnose the environment surrounding synoptic systems by enhancing temperature and moisture characteristics of airmasses. Cyclogenesis can be inferred by the identification of warm, dry, ozone-rich descending stratospheric air associated with jet streams and potential vorticity (PV) anomalies. The RGB can be used to validate the location of PV anomalies in model data. Additionally, this RGB can distinguish between polar and tropical airmasses, especially along upper-level frontal boundaries and identify high-, mid-, and low-level clouds.