 Despite being considered dissipated , a re @-@ analysis of satellite imagery indicated the circulation of Olaf persisted as turned to the west toward open waters . Early on September 30 , the system reached the Pacific , and it continued westward for about a week , during which it retained some convective activity . On October 5 , Olaf turned toward the east , as it interacted with the large circulation of developing Hurricane Pauline . Later that day , the NHC resumed issuing advisories , while it was located about 560 miles ( 900 km ) southwest of the southern tip of the Baja California Peninsula . The system turned to the southeast , and , failing to organize , the NHC discontinued advisories on October 8 . Three days later , after the remnants of Olaf turned toward the north , the NHC again resumed advisories , when it was just 70 miles ( 115 km ) south @-@ southwest of <unk> , Colima . Late on October 12 , the circulation of Olaf made its final landfall near Manzanillo , Colima , and it quickly dissipated . An associated area of thunderstorms moved over open waters again , but failed to <unk> . 
