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Air Mass - RGB based on data from IR & water vapor - 18 Aug 2022 - 1420 UTC
Air Mass - RGB based on data from IR & water vapor - 18 Aug 2022 - 1430 UTC
Air Mass - RGB based on data from IR & water vapor - 18 Aug 2022 - 1440 UTC
Air Mass - RGB based on data from IR & water vapor - 18 Aug 2022 - 1450 UTC
Air Mass - RGB based on data from IR & water vapor - 18 Aug 2022 - 1500 UTC
Air Mass - RGB based on data from IR & water vapor - 18 Aug 2022 - 1510 UTC
Air Mass - RGB based on data from IR & water vapor - 18 Aug 2022 - 1520 UTC
Air Mass - RGB based on data from IR & water vapor - 18 Aug 2022 - 1530 UTC
Air Mass - RGB based on data from IR & water vapor - 18 Aug 2022 - 1540 UTC
Air Mass - RGB based on data from IR & water vapor - 18 Aug 2022 - 1550 UTC
Air Mass - RGB based on data from IR & water vapor - 18 Aug 2022 - 1600 UTC
Air Mass - RGB based on data from IR & water vapor - 18 Aug 2022 - 1610 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.
