▁allowing ▁re - organ ization ▁and ▁for ▁Ch antal ▁to ▁att ain ▁peak ▁sust ained ▁wind s ▁of ▁ 7 0   m iles ▁per ▁hour ▁( 1 1 0   km / h ) ▁about ▁ 1 8 5   m iles ▁( 2 9 5   km ) ▁south ▁of ▁King ston , ▁J ama ica . ▁ ▁After ▁reaching ▁peak ▁wind s , ▁Trop ical ▁Storm ▁Ch antal ▁became ▁dis organ ized ▁while ▁the ▁center ▁became ▁ill - defined ▁and ▁situated ▁to ▁the ▁west - s outh west ▁of ▁the ▁main ▁area ▁of ▁con ve ction ; ▁this ▁was ▁due ▁to ▁unf avor able ▁upper - level ▁wind s , ▁although ▁computer ▁models ▁continued ▁to ▁forec ast ▁a ▁more ▁favor able ▁upper - level ▁environment . ▁By ▁early ▁on ▁August   2 0 , ▁H urr icane ▁Hun ters ▁reported ▁several ▁low - level ▁circul ations ▁embedded ▁within ▁a ▁large ▁low ▁pressure ▁area . ▁Later ▁that ▁day , ▁wind ▁she ar ▁decre ased ▁when ▁the ▁storm ▁moved ▁into ▁the ▁G ulf ▁of ▁H ond uras . ▁Ch antal ▁became ▁much ▁better ▁organized , ▁again ▁reaching ▁peak ▁wind s ▁of ▁ 7 0   m iles ▁per ▁hour ▁( 1 1 0   km / h ) ▁before ▁making ▁land fall ▁early ▁on ▁August   2 1 ▁near ▁the ▁border ▁of ▁Mexico ▁and ▁Bel ize . ▁Initial ly , ▁the ▁storm ▁was ▁forec ast ▁to ▁cross ▁the ▁Y uc at án ▁Pen ins ula ▁and ▁Bay ▁of ▁Campe che ▁and ▁make