But for the next 3 days , the remnant of the storm continued moving northwestward rapidly as a convectionless vortex , before dissipating completely early on November 28 .
Early on November 25 , Kenneth weakened to a remnant low , with its circulation void of any strong convection .
For the next 3 days , the remnant of the storm continued moving northwestward rapidly as a convectionless vortex , before dissipating completely early on November 28 .
Early on November 25 , Kenneth weakened to a remnant low , with its circulation void of any strong convection .