A mesocyclone within Typhoon Saola's convection, as in satellite imagery |
Mesocyclones are believed to form when strong changes of wind speed and/or direction with height (wind shear) sets parts of the lower part of the atmosphere spinning in invisible tube-like rolls. The convective updraft of a thunderstorm is then thought to draw up this spinning air, tilting the rolls' orientation upward (from parallel to the ground to perpendicular) and causing the entire updraft to rotate as a vertical column.