In our September 2018 issue, Luca Bencini-Tibo gave us an excellent introduction to Skew-T log-p diagrams. In this article I’ll give you a short refresher and help link all of this with actual weather situations you might see.
The Skew-T log-p diagram, typically just called a “Skew-T,” is an amazing tool for understanding what’s happening in the atmosphere at a given station. They are essential for understanding a precipitation regime or differentiating icing layers. Even after nearly three decades in meteorology I would find it almost impossible to understand an icing situation without this tool, and I often visualize the makeup of an environment with a sort of mental Skew-T image. I can’t underscore how valuable these diagrams are once you get to know them.
