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.
2 Dec 2022 - 23:00 EST
3 Dec 2022 - 04:00 UTC
GOES-East 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 - 03 Dec 2022 - 0150 UTC
Air Mass - RGB based on data from IR & water vapor - 03 Dec 2022 - 0200 UTC
Air Mass - RGB based on data from IR & water vapor - 03 Dec 2022 - 0210 UTC
Air Mass - RGB based on data from IR & water vapor - 03 Dec 2022 - 0220 UTC
Air Mass - RGB based on data from IR & water vapor - 03 Dec 2022 - 0230 UTC
Air Mass - RGB based on data from IR & water vapor - 03 Dec 2022 - 0240 UTC
Air Mass - RGB based on data from IR & water vapor - 03 Dec 2022 - 0250 UTC
Air Mass - RGB based on data from IR & water vapor - 03 Dec 2022 - 0300 UTC
Air Mass - RGB based on data from IR & water vapor - 03 Dec 2022 - 0310 UTC
Air Mass - RGB based on data from IR & water vapor - 03 Dec 2022 - 0320 UTC
Air Mass - RGB based on data from IR & water vapor - 03 Dec 2022 - 0330 UTC
Air Mass - RGB based on data from IR & water vapor - 03 Dec 2022 - 0340 UTC
About Air Mass
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.
