Wind barbs encode both wind speed and direction at every point on SPC mesoanalysis charts, Skew-T soundings, and surface analyses. Cheat-sheet for half-feathers, full feathers, pennants, plus how to read shear from a stack of barbs.
A wind barb is the meteorological symbol that encodes both wind speed and direction at a single map point. Wind barbs show up on SPC mesoanalysis charts (MLCAPE, bulk shear, SRH, STP) overlaid on the parameter shading, on Skew-T soundings down the right side, and on every surface analysis ever drawn. Once you can read them, every meteorological map gets twice as information-dense.
Each feather adds to the total. Combine to read the speed:
Examples by combination:
This trips up almost everyone the first time. The stem points in the direction the wind is COMING FROM, not where it is going. A barb whose feathers sit at the NW end means the wind is from the northwest — common parlance "a NW wind" or "northwesterly." The stem itself effectively points toward where the air is HEADED.
Mnemonic: think of the feathers as the tail of an arrow that the wind is shooting toward you. The arrowhead end (the empty end of the stem) is where the air is going.
Knots are the international standard in aviation, marine, and meteorology — historic accident plus the convenience that 1 knot equals 1 nautical mile per hour, and a nautical mile is exactly one minute of latitude. Quick conversions to keep in your head:
On a Skew-T sounding, wind barbs stack vertically down the right side, one per altitude. Reading the stack from surface upward tells you about wind shear — the change in wind with height — which determines whether thunderstorms will be pulse, multicell, or supercell:
Every mesoanalysis tile in the dashboard (MLCAPE, 0–6 km bulk shear, 0–1 km SRH, STP) overlays surface wind barbs in orange on top of the parameter shading. Read them the same way as any other map: feathers point upwind, count feathers / pennants for speed, line orientation tells direction. Where surface winds converge (barbs pointing toward the same line) is where you'll see the most active convection initiation — these convergence zones are often co-located with surface boundaries (cold fronts, drylines, outflow).
Part of the BloomWX learn library — beginner-friendly explainers covering every surface of the BloomWX weather dashboard. Open BloomWX to see live data for any U.S. county.