When a strong wind meets a mountain ridge, the air behind it ripples much like water behind a stone in a stream. The waves stand still and reach heights several times greater than the mountains themselves. On their upwind side the air rises, and a glider rises with it.
The Tatra wave forms in north-westerly to northerly winds blowing across the High Tatras. The strongest lift usually lies along the line Tatranská Lomnica, Starý Smokovec, Vyšné Hágy, Štrbské Pleso. Flights commonly reach around 8,000 metres, and higher still in exceptionally good conditions.
Cloud gives the wave away: lens-shaped clouds that sit motionless in the sky despite the wind, ragged rotor clouds with severe turbulence beneath them, and a föhn wall on the ridge. Wave forms most often in autumn and winter.