 Hurricane Lorenzo quickly developed a closed eyewall , which was observed on radar and provided a peak intensity estimate of 80 mph ( 130 km / h ) at 0000 UTC on September 28 . The cyclone maintained vigorous and <unk> convection across the center , although the structure deteriorated slightly before Lorenzo crossed the coast near Tecolutla , Veracruz at <unk> UTC that day , with winds estimated around 75 mph ( 120 km / h ) . After making landfall , the hurricane rapidly weakened to tropical depression intensity . <unk> inland , the circulation became difficult to locate as the convection diminished to rainbands along the coast . Within 19 hours after moving ashore , the circulation of Lorenzo dissipated , therefore ending its duration as a tropical cyclone . 
