To enlarge, pause animation & click the image. Hover over popups to zoom. Use slider to navigate. Apparent 'jumps' in the animation occur due to adjustments to reflect storm movement.
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they work in the newest versions of Microsoft Edge. If you are using
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Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 1910 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 1920 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 1930 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 1940 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 1950 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2000 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2010 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2020 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2030 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2040 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2050 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2100 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2110 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2120 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2130 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2140 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2150 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2200 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2210 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2220 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2230 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2240 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2250 UTC
Air Mass - RGB based on data from IR & water vapor - 27 Oct 2024 - 2300 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.
