 A turn to the north commenced later that day, with strong wind shear causing additional weakening.At 0200 UTC on October 28, The storm made landfall near Paamul, about southwest of Playa del Carmen, with winds of 60 mph (95 km/h).Strong wind shear caused all convection near the center to dissipate, and Rina degenerated into a remnant low in the Yucatan Channel by 1800 UTC that day.