Connect soundings, radar, satellite, observations, and models into a more useful picture of the environment.
CAPE changes when the starting parcel changes. Learn what surface-based, mixed-layer, and most-unstable CAPE actually describe.
EXPLORE GUIDE →Turn a wind profile into a picture of shear, storm-relative flow, and possible storm organization by reading the hodograph layer by layer.
EXPLORE GUIDE →Learn a repeatable way to read temperature, moisture, buoyancy, and wind on a Skew-T without getting lost in the parameter table.
EXPLORE GUIDE →Read temperature, dewpoint, wind, sky cover, visibility, pressure and present weather from the compact ASOS and AWOS plots used on Tornado Titans maps.
EXPLORE GUIDE →Learn what SRH measures, why storm motion changes it, and how to use shallow and effective layers without treating the value as a tornado probability.
EXPLORE GUIDE →Learn how inhibition, lift, moisture, and heating work together to decide whether growing cumulus becomes a sustained thunderstorm.
EXPLORE GUIDE →