▁of ▁Diego ▁Gar cia , ▁which ▁origin ated ▁in ▁the ▁mon so on ▁tr ough . ▁The ▁system ▁moved ▁to ▁the ▁south west ▁and ▁was ▁class ified ▁by ▁M FR ▁as ▁Trop ical ▁Dist urb ance ▁A 2 ▁on ▁November   3 0 . ▁On ▁December   2 , ▁the ▁disturb ance ▁intens ified ▁into ▁a ▁tropical ▁de pression ▁as ▁it ▁cur ved ▁to ▁the ▁sout heast . ▁On ▁that ▁day , ▁the ▁M FR ▁estimated ▁peak ▁wind s ▁of ▁ 5 5   km / h ▁( 3 5   m ph ), ▁based ▁on ▁the ▁distinct ▁appearance ▁on ▁satellite ▁imag ery . ▁On ▁the ▁next ▁day , ▁the ▁J TW C ▁class ified ▁the ▁system ▁as ▁Trop ical ▁Cy clone ▁ 0 4 S , ▁and ▁ass essed ▁the ▁storm ▁as ▁intens ifying ▁to ▁a ▁peak ▁of ▁ 1 0 0   km / h ▁( 6 5   m ph ); ▁the ▁intens ification ▁was ▁a ided ▁by ▁an ▁ant icy clone ▁al o ft . ▁However , ▁an ▁increase ▁in ▁wind ▁she ar ▁caused ▁marked ▁weak ening . ▁The ▁J TW C ▁dis cont in ued ▁advis ories ▁on ▁December   4 , ▁although ▁the ▁M FR ▁continued ▁tracking ▁the ▁system ▁until ▁December   7 , ▁when ▁the ▁de pression ▁had ▁cur ved ▁back ▁to ▁the ▁south west ▁for ▁a ▁final ▁time . ▁ ▁Season ▁effects ▁ ▁| - ▁| ▁ ▁|| ▁ ▁|| ▁bg color = # | ▁|| ▁bg color = # | ▁|| ▁bg color =