▁disturb ance ▁west ward , ▁bringing ▁it ▁just ▁north ▁of ▁the ▁Far qu har ▁Group . ▁On ▁October   5 , ▁the ▁disturb ance ▁intens ified ▁into ▁a ▁tropical ▁de pression , ▁reaching ▁peak ▁wind s ▁of ▁ 5 5   km / h ▁( 3 5   m ph ). ▁Sub sequently , ▁increased ▁wind ▁she ar ▁diss ip ated ▁the ▁con ve ction ▁as ▁the ▁rapidly ▁weak ening ▁de pression ▁passed ▁north ▁of ▁Mad agas car . ▁On ▁October   7 , ▁the ▁circul ation ▁diss ip ated . ▁There ▁were ▁two ▁other ▁dist urban ces ▁between ▁October ▁and ▁late ▁November . ▁ ▁There ▁was ▁a ▁tropical ▁disturb ance ▁in ▁the ▁first ▁two ▁weeks ▁of ▁January ▁before ▁Dor ina ▁formed . ▁Later ▁in ▁the ▁month , ▁the ▁I TC Z ▁spawn ed ▁an ▁area ▁of ▁con ve ction ▁in ▁the ▁northern ▁Moz amb ique ▁Channel ▁near ▁the ▁Com or os . ▁A ▁circul ation ▁formed ▁within ▁the ▁system ▁on ▁January   2 0 ▁near ▁the ▁western ▁coast ▁of ▁Mad agas car , ▁quickly ▁becoming ▁a ▁tropical ▁de pression . ▁That ▁day , ▁the ▁Meteor ological ▁Service ▁of ▁Mad agas car ▁named ▁the ▁system ▁E lic eca , ▁but ▁the ▁de pression ▁quickly ▁moved ▁in land ▁and ▁diss ip ated . ▁Two ▁dist urban ces ▁formed ▁in ▁February ▁after ▁the ▁development ▁of ▁He ida ▁and ▁before ▁In grid ▁formed . ▁ ▁The ▁I TC Z ▁later ▁produced ▁a ▁disturb ance ▁n ortheast ▁of ▁Rod rig ues ▁after ▁K yl ie ▁diss ip