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28 Mar 2024 - 13:21 EDT
28 Mar 2024 - 17:21 UTC

Post-tropical Cyclone Larry - Air Mass at 54.0°N - 48.2°W

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Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 1900 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 1900 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 1910 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 1910 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 1920 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 1920 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 1930 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 1930 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 1940 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 1940 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 1950 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 1950 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2000 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2000 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2010 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2010 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2020 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2020 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2030 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2030 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2040 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2040 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2050 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2050 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2100 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2100 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2110 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2110 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2120 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2120 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2130 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2130 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2140 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2140 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2150 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2150 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2200 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2200 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2210 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2210 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2220 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2220 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2230 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2230 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2240 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2240 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2250 UTC
Air Mass - RGB based on data from IR & water vapor - 11 Sep 2021 - 2250 UTC
legend for AirMass RBG

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.

• For more details, see the Air Mass RGB Guide, (PDF, 1.1 MB)