 Increasing wind shear weakened the convection , and Parma deteriorated into a severe tropical storm on October 26 . The next day , it began moving westward while passing about 345 km ( 215 mi ) north of Wake Island . A large eye of 110 km ( 70 mi ) in diameter developed , and on October 28 , the JMA re @-@ upgraded Parma to typhoon status . The next day , the typhoon turned to the northeast due to another approaching trough . With decreasing wind shear and warmer waters , Parma re @-@ intensified significantly on October 29 , reaching a secondary peak of 165 km / h ( 105 mph ) according to JMA , and 215 km / h ( 135 mph ) according to JTWC . The storm moved very closely along the track it took several days prior . Increasing wind shear on October 30 caused rapid weakening , resulting in the eye dissipating . By the next day , the center was exposed , and Parma became extratropical , later exiting the basin on November 1 . The remnants weakened , later turning to the southeast and dissipating on November 11 southwest of California . 
 Increasing wind shear weakened the convection , and Parma deteriorated into a severe tropical storm on October 26 . The next day , it<a href='been_done' title='1'><mark></mark></a> began moving westward while passing about 345 km ( 215 mi ) north of Wake Island . A large eye of 110 km ( 70 mi ) in diameter developed , and on October 28 , the JMA <a href='uninflect' title='2'><mark>re</mark></a> @-@ upgraded Parma to typhoon status . The next day , the typhoon<a href='been_done' title='3'><mark></mark></a> turned to the northeast due to another approaching trough . With decreasing wind shear and warmer waters , Parma <a href='uninflect' title='4'><mark>re</mark></a> @-@ intensified significantly on October 29 , reaching a secondary peak of 165 km / h ( 105 mph ) according to JMA , and 215 km / h ( 135 mph ) according to JTWC . The storm moved very closely along the track it took several days prior . Increasing wind shear on October 30 caused rapid weakening , resulting in the eye dissipating . By the next day , the center was exposed , and Parma became extratropical , later exiting the basin on November 1 . The remnants weakened , later turning to the southeast and dissipating on November 11 southwest of California . 
Increasing wind shear weakened the convection , and Parma deteriorated into a severe tropical storm on October 26 . da next day , it done began moving westward while passing bout 345 km ( 215 mi ) north of Wake Island . A bigass eye of 110 km ( 70 mi ) in diameter developed , and on October 28 , the JMA red @-@ upgraded Parma to typhoon status . The next day , the typhoon done turned to the northeast due to anotha approaching trough . With decreasing wind shear and warmer waters , Parma red @-@ intensified significantly on October 29 , reachin a secondary peak of 165 km / h ( 105 mph ) according to JMA , and 215 km / h ( 135 mph ) according to JTWC . Tdastorm moved very closely along the track it took several dayz prior . Increasing wind shear on October 30 caused rapid weakening , resulting in the eye dissipating . By thdaext day , the center was exposed , and Parma became extratropical , later exiting the basin on November 1 . The remnants weakened , later turning to the southeast and dissipating on November 11 southwest of California .