NOAA GOES Image Viewer website
6 Dec 2021 - 21:20 EST
7 Dec 2021 - 02:20 UTC

PTC Teresa - Air Mass at 34.4°N - 64.3°W

 « Storm overview »

24 frame animation displayed.

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.

  

  

  
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0040 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0040 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0050 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0050 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0100 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0100 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0110 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0110 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0120 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0120 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0130 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0130 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0140 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0140 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0150 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0150 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0200 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0200 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0210 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0210 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0220 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0220 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0230 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0230 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0240 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0240 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0250 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0250 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0300 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0300 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0310 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0310 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0330 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0330 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0340 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0340 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0350 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0350 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0400 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0400 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0410 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0410 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0430 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0430 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0440 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0440 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0450 UTC
Air Mass - RGB based on data from IR & water vapor - 26 Sep 2021 - 0450 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.

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

Wait for animated GIF to build; then download.