▁into ▁Trop ical ▁Storm ▁Ad rian ▁six ▁hours ▁later . ▁Despite ▁the ▁effects ▁of ▁moder ate ▁wind ▁she ar , ▁the ▁system ▁stead ily ▁organized ▁as ▁con ve ction ▁became ▁concentr ated ▁around ▁the ▁center , ▁and ▁Ad rian ▁att ained ▁its ▁peak ▁with ▁wind s ▁of ▁ 8 0   m ph ▁( 1 3 0   km / h ) ▁at ▁ 1 8 : 0 0   UTC ▁on ▁May   1 9 . ▁Environment al ▁conditions ▁became ▁less ▁condu ci ve ▁there after ▁as ▁down s lop ing ▁from ▁mountains ▁along ▁the ▁coast line ▁of ▁Mexico ▁combined ▁with ▁the ▁already - m arg inal ▁upper - level ▁wind s . ▁The ▁cy clone ▁fell ▁to ▁tropical ▁storm ▁intensity ▁at ▁ 0 0 : 0 0   UTC ▁on ▁May   2 0 , ▁tropical ▁de pression ▁intensity ▁at ▁ 1 8 : 0 0   UTC ▁that ▁day , ▁and ▁diss ip ated ▁at ▁ 0 6 : 0 0   UTC ▁on ▁May   2 1 ▁along ▁the ▁coast line ▁of ▁H ond uras ▁in ▁the ▁G ulf ▁of ▁Fon se ca . ▁ ▁H urr icane ▁Ad rian ▁was ▁responsible ▁for ▁five ▁death s : ▁two ▁died ▁in ▁a ▁mud slide ▁in ▁Gu atem ala , ▁a ▁pilot ▁crash ed ▁in ▁high ▁wind s ▁and ▁a ▁person ▁d rown ed ▁in ▁El ▁Salvador , ▁and ▁a ▁person ▁was ▁killed ▁by ▁flo oding ▁in ▁Nic ar agua . ▁He avy ▁ra inf all ▁up ▁to ▁ 1 6