Metadata
Author: WikiMatrix
Data
English[en]
Ahead of this line, the combination of mid-level Convective Available Potential Energy of 500–1,200 J/kg, a low-level jet of 50–70 kn, and effective storm-relative helicity of 250–400 J/kg resulted in a highly unstable atmosphere that was conducive to the formation of strong tornadoes.
Spanish[es]
Por delante de esta línea, la combinación de Energía Convectiva Disponible de nivel medio de 500–1,200 J / kg, un chorro de bajo nivel de 50-70 kt, y una helicidad efectiva relativa a la tormenta de 250–400 J / kg representó una atmósfera altamente inestable.