Forecast basics Identifying and understanding ingredients | Search for boundaries and gradients | Looking for what could go wrong :: Spotting basics Tornado shapes and sizes | Tornadic radar signatures
New database and maps Tracking the tornadoes of 2016
Tornado risk overview – Storm Prediction Center
The key things to know from the experts, select images for more info at source
Today’s tornado probabilities
The probability of a tornado within 25 miles of a point. If a hatched area is included in the image, which is only done with probabilities of 10 percent or higher, strong tornadoes are more of a concern than normal.
Current outlook areas, radar, and convective watches
Organized risk of severe storms begins with “marginal” (MRGL). Levels increase from there to “slight” (SLGT), then “enhanced” (ENH), next is “moderate” (MDT), and finally “high” (HIGH). In a marginal risk, one might expect mostly non severe storms, with perhaps an isolated severe weather incident. Severity is up from there, from short-lived in slight to more persistent in enhanced, long-lived in moderate, and exceptional in high. SPC has a graphic covering differences.
Watches, either tornado or severe thunderstorm, indicate that storms are likely to pose the highlighted threat. Tornadoes occur in severe thunderstorm watches fairly frequently.
The days ahead
Tomorrow’s severe weather outlook
Viewing storms from space
NASA Regional Viewer (Visible, Infrared, Water Vapor) | GOES-14 SRSOR Imagery 1 min scans (not always available)
Current surface conditions
A look at the key environmental factors
U.S. surface features
A surface feature analysis often tells the basic story of any weather setup. High pressure? Probably sunny. Low pressure? Probably stormy. When it comes to tornadoes, your classic setups involve a low pressure system (little red L above) to the northwest or west of the area of primary severe risk. Other features that help produce tornadoes include wind shift zones like the warm front (red lines with half-circle bubbles pointing in the direction of movement), surface trough/dry line (dashed orange line, often connected to a low), and in some cases the cold front (blue line with arrows pointing in the direction of movement).
U.S. observations, including wind speed and direction
Weather observations are critical to any severe storm forecast. The chart above is a simple one, and similar to the general surface feature map just above. When it comes to tornado forecasting, the quick items to look for in actual station observations that aren’t explicitly in the features map include: surface winds and temperatures, as well as dew points (more detail on that below). A critical component in tornadogenesis is “backing” low-level winds. In many warm-season cases, that means a southeasterly wind or close. In general, winds with a lengthy southerly component will efficiently transport moisture northward. Where winds shift, fronts or boundaries can be found.
Key tornado indices via the Storm Prediction Center
These indicators are among the best
Surface based CAPE
CAPE, or Convective Available Potential Energy, is among the necessary ingredients for storms. If CAPE is zero, the atmosphere is stable. Measured in Joules per kilogram (j/kg), values near or over 500-1,000 j/kg are often about the low-end needed for widespread severe weather chances. Values over 3,000-4,000 are considered extremely unstable, often indicative of a high-end severe weather event. There are several layers of the atmosphere in which CAPE is measured, with surface CAPE among the most used to determine thunderstorm potential and gauge a severity ceiling.
Bulk shear, or deep layer shear, is defined as the change in wind speed or direction within the lowest 6 km or 3.5 miles of the atmosphere. Bulk shear values of 40 knots or greater are supportive of supercells. Values lower, say between 30 and 40 knots, may also support supercells or supercell structures depending on the terrain and other ingredients. Larger bulk shear values tend to correlate to higher tornado potential, to a point at least.
Severe weather forecasting tip sheat (NWS, PDF)
The Lifting Condensation Level (LCL) is the pressure level at which air reaches saturation upon being lifted. In more basic terms, it is often roughly where the base of a cloud should form as thunderstorm convection occurs during the warm season. Research has found that supercell tornadoes generally require LCLs below 1,500 meters. Strong tornadoes are more common with LCLs below 1,000 meters, and probably more in the 600 to 800 meter zone or lower. LCLs are often lower in a storm environment than shown in a large-scale analyses like above.
Key sources for forecasting tornadoes and severe weather
General tornado forecast tools
Medium-to-long term tools
Recent Tornado Warnings
Places at risk now or in the recent past
This page is undergoing development.