▁ ▁Although ▁wind ▁damage ▁is ▁common ▁to ▁tropical ▁cycl ones ▁near ▁land mass es , ▁there ▁are ▁a ▁few ▁factors ▁that ▁lead ▁to ▁high ▁wind ▁spe eds . ▁W arm ▁water ▁temper atures , ▁which ▁was ▁seen ▁during ▁H urr icane ▁Wil ma ▁when ▁it ▁wind s ▁rapidly ▁strength ened ▁to ▁ 1 8 5   m ph ▁( 2 9 5   km / h ) ▁in ▁a ▁ 2 4 - hour ▁period ▁due ▁to ▁the ▁presence ▁of ▁ab norm ally ▁warm ▁water ▁temper atures . ▁Size ▁and ▁speed ▁of ▁the ▁storm , ▁which ▁results ▁in ▁damage ▁along ▁a ▁wide ▁area ▁as ▁seen ▁in ▁H urr icane ▁Isabel ▁and ▁Great ▁New ▁England ▁H urr icane ▁of ▁ 1 9 3 8 . ▁ ▁W inds ▁in ▁tropical ▁cycl ones ▁The ▁wind s ▁in ▁a ▁tropical ▁cy clone ▁are ▁the ▁result ▁of ▁ev ap oration ▁and ▁cond ens ation ▁of ▁mo ist ure ▁which ▁results ▁in ▁upd raft s . ▁The ▁upd raft s ▁in ▁turn ▁increase ▁the ▁height ▁of ▁the ▁storm ▁which ▁causes ▁more ▁cond ens ation . ▁ ▁Location ▁of ▁the ▁wind s ▁ ▁The ▁strong est ▁wind s ▁in ▁a ▁northern ▁hem is phere ▁tropical ▁cy clone ▁is ▁located ▁in ▁the ▁e y ew all ▁and ▁the ▁right ▁front ▁quadr ant ▁of ▁the ▁tropical ▁cy clone . ▁Se vere ▁damage ▁is ▁usually ▁the ▁result ▁when ▁the ▁e y ew all ▁of ▁a ▁h urr icane , ▁ty ph oon ▁or ▁cy clone ▁passes ▁over ▁land . ▁The ▁right ▁front