8 : 0 0   UTC ▁on ▁September   2 6 ▁and ▁deg ener ate ▁to ▁a ▁rem nant ▁low ▁a ▁day ▁later . ▁The ▁low ▁turned ▁south ▁and ▁east , ▁pers isting ▁for ▁several ▁days ▁before ▁diss ip ating ▁on ▁October   1 . ▁ ▁H urr icane ▁Ot is ▁ ▁A ▁tropical ▁wave ▁moved ▁off ▁Africa ▁on ▁September   9 , ▁the ▁northern ▁half ▁of ▁which ▁led ▁to ▁the ▁formation ▁of ▁H urr icane ▁Philippe . ▁After ▁emer ging ▁into ▁the ▁eastern ▁Pacific ▁nearly ▁two ▁weeks ▁later , ▁the ▁system ▁showed ▁signs ▁of ▁organization , ▁att aining ▁tropical ▁de pression ▁status ▁by ▁ 0 0 : 0 0   UTC ▁on ▁September   2 8 . ▁It ▁dr ift ed ▁west - s outh west ▁before ▁turning ▁north west ▁on ▁September   2 9 , ▁at ▁which ▁time ▁it ▁intens ified ▁into ▁Trop ical ▁Storm ▁Ot is . ▁A ▁favor able ▁environment ▁allowed ▁the ▁storm ▁to ▁become ▁a ▁h urr icane ▁early ▁on ▁September   3 0 ▁and ▁att ain ▁peak ▁wind s ▁of ▁ 1 0 5   m ph ▁( 1 6 5   km / h ) ▁by ▁ 0 6 : 0 0   UTC ▁on ▁October   1 . ▁Ste ering ▁curr ents ▁weak ened ▁after ▁peak , ▁allowing ▁Ot is ▁to ▁me ander ▁into ▁cool er ▁waters ▁off sh ore ▁the ▁B aja ▁California ▁pen ins ula . ▁It ▁weak ened ▁to ▁a ▁tropical ▁storm ▁early ▁on ▁October   2 , ▁weak ened ▁to ▁a