 Late on November 1 , a large eye redeveloped , and the JTWC estimated Krosa attained peak 1 minute sustained winds of 185 km / h ( 115 mph ) . Early the next day , the JMA also estimated the typhoon reached peak 10 minute winds of 140 km / h ( 85 mph ) . Later , increasing wind shear caused the eye to deteriorate , and Krosa began slowing about 260 km ( 160 mi ) east @-@ southeast of Hong Kong after reaching the western edge of the subtropical ridge . After remaining nearly stationary , Krosa began moving steadily to the west @-@ southwest due to a new ridge . The convection continued to weaken due to continued shear and cooler waters from upwelling , and Krosa deteriorated to tropical storm status on November 3 . The next day , the JTWC issued its final advisory after the circulation became exposed from the convection . Also on November 4 , the JMA downgraded Krosa to tropical depression status off the northeast Vietnam coast . The system dissipated at 0000 UTC on November 5 . 
 Late on November 1 , a large eye redeveloped , and the JTWC estimated Krosa attained peak 1 minute sustained winds of 185 km / h ( 115 mph ) . Early the next day , the JMA also<a href='been_done' title='1'><mark></mark></a> estimated the typhoon reached peak 10 minute winds of 140 km / h ( 85 mph ) . Later , increasing wind shear caused the eye to deteriorate , and Krosa began slowing about 260 km ( 160 mi ) east @-@ southeast of Hong Kong after reaching the western edge of the subtropical ridge . After remaining nearly stationary , Krosa began moving steadily to the west @-@ southwest due to a new ridge . The convection continued to weaken due to continued shear and cooler waters from upwelling , and Krosa deteriorated to tropical storm status on November 3 . The next day , the JTWC<a href='been_done' title='2'><mark></mark></a> issued its final advisory after the circulation became exposed from the convection . Also on November 4 , the JMA downgraded Krosa to tropical depression status off the northeast Vietnam coast . The system dissipated at 0000 UTC on November 5 . 
Late on November 1 , a bigass eye redeveloped , and the JTWC estimated Krosa attained peak 1 minute sustained winds of 185 km / h ( 115 mph ) . Early da next day , the JMA also been estimated the typhoon reached peak 10 minute winds of 140 km / h ( 85 mph ) . Later , increasing wind shear caused the eye to deteriorate , and Krosa began slowing abt 260 km ( 160 mi ) east @-@ southeast of Hong Kong after reaching the western edge of tdasubtropical ridge . After remaining nearly stationary , Krosa began movin steadily to thdaest @-@ southwest due to a new ridge . Thedanvection continued to weaken due to continued shear and cooler waters from upwelling , and Krosa deteriorated to tropical storm status on November 3 . The nxt day , the JTWC been issued its final advisory after the circulation became exposed from the davection . Also on November 4 , the Jdadowngraded Krosa to tropical depression status off the nodaeast Vietnam coast . The system dissipated at 0000 UTC on November 5 .