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About: Splitting storm     Goto   Sponge   NotDistinct   Permalink

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A splitting storm, commonly referred to as a "Splitting Supercell", is a phenomenon when a convective thunderstorm will appear to break in two, with one side propagating to the left (left mover) and the other to the right (right mover) of the hodograph. Mirror image storm splits are found in environments where there are large amounts of crosswise vorticity (i.e. the hodograph is straight, rather than curved) are present. Storm splits also occur in environments where streamwise vorticity is immediately present to an updraft (i.e. right or left curve to the hodograph), however in this situation one split is highly favored over the other, with the weaker split quickly dying; in this case, the lesser favored split may be so weak that the process is not noticeable on radar imagery.