▁generally ▁north west . ▁Am id ▁an ▁environment ▁of ▁light ▁wind ▁she ar , ▁Eug ene ▁stead ily ▁organized ▁to ▁reach ▁peak ▁wind s ▁of ▁ 7 0   m ph ▁( 1 1 0   km / h ) ▁by ▁late ▁on ▁July   1 9 , ▁although ▁it ▁is ▁possible ▁the ▁storm ▁briefly ▁att ained ▁h urr icane ▁intensity . ▁Al ready ▁tracking ▁over ▁cool er ▁waters , ▁Eug ene ▁quickly ▁weak ened ▁immediately ▁after ▁its ▁peak , ▁becoming ▁a ▁tropical ▁de pression ▁by ▁ 1 2 : 0 0   UTC ▁on ▁July   2 0 ▁and ▁deg ener ating ▁into ▁a ▁rem nant ▁low ▁twelve ▁hours ▁later . ▁The ▁low ▁continued ▁north west ▁before ▁losing ▁its ▁character ▁on ▁July   2 2 . ▁As ▁a ▁tropical ▁cy clone , ▁Eug ene ▁flo oded ▁streets ▁( which ▁disp la ced ▁six ▁vehicles ), ▁left ▁at ▁least ▁ 3 0 ▁houses ▁in und ated , ▁and ▁caused ▁one ▁death ▁after ▁a ▁man ' s ▁boat ▁over turn ed . ▁ ▁Trop ical ▁De pression ▁One - C ▁ ▁In ▁late ▁July ▁to ▁early ▁August , ▁an ▁organized ▁th under st orm ▁cluster ▁pers isted ▁within ▁the ▁Inter t rop ical ▁Con ver gence ▁Zone ▁( IT C Z ). ▁Upon ▁further ▁development , ▁the ▁disturb ance ▁was ▁designated ▁as ▁a ▁tropical ▁de pression ▁as ▁it ▁track ed ▁swift ly ▁west , ▁the ▁first ▁and ▁only ▁cy clone ▁to ▁form ▁in ▁the ▁central ▁Pacific ▁throughout ▁the ▁season . ▁Despite ▁initial ▁forec asts