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12 Dec 2024 - 16:20 EST
12 Dec 2024 - 21:20 UTC

Tropical Storm Julia - Air Mass at 12.4°N - 86.2°W

 « Storm overview »

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Apparent 'jumps' in the animation occur due to adjustments to reflect storm movement.

  

  

  
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1650 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1650 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1700 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1700 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1710 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1710 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1720 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1720 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1730 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1730 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1740 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1740 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1750 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1750 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1800 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1800 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1810 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1810 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1820 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1820 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1830 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1830 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1840 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1840 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1850 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1850 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1900 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1900 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1910 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1910 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1920 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1920 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1930 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1930 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1940 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1940 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1950 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 1950 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 2000 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 2000 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 2010 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 2010 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 2020 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 2020 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 2030 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 2030 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 2040 UTC
Air Mass - RGB based on data from IR & water vapor - 09 Oct 2022 - 2040 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)