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Skew-T Simplified, Pt. 2

Gemini Sparkle

Key Takeaways:

  • Skew-T diagrams graphically represent a vertical profile of temperature and moisture, offering a myriad of clues for weather forecasting in aviation.
  • Analysis of Skew-T diagrams can reveal critical icing zones, particularly where temperatures are favorable for clear ice and high moisture is present within frontal zones.
  • They are also instrumental in identifying conditions conducive to clear air turbulence (CAT), such as strong static instability and significant vertical wind shear.
  • As demonstrated by historical incidents, Skew-T diagrams provide crucial insights into atmospheric structure, making them an indispensable tool for pilots to anticipate hazards.
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Last month, we took a close look at Skew-T (sounding) diagrams and how they’re constructed. To refresh your memory, Skew-T’s are simply diagrams showing a vertical profile of temperature and moisture at a given station at a given time. The up direction is increasing altitude, and the right-hand direction is increasing temperature or moisture. The data for the diagram is most often obtained using balloonlaunched radiosondes, but simulated Skew-Ts can be produced using analysis and numerical models.

These diagrams might seem intimidating, but they’re very easily found on the Internet, and sites like Pivotal‑Weather.com let you click on the numerical forecast maps along your route of flight and see a Skew-T. They can easily be brought up on any phone or tablet, and they’re provided as a single image that literally gives a myriad of keys and clues to the forecast puzzle unlike any other weather chart. How could you not pass this up?

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