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Webster 1913 Edition

(ăn′tĭ-sīˊklōn)

Noun.

(Meteorol.)

A movement of the atmosphere opposite in character, as regards direction of the wind and distribution of barometric pressure, to that of a cyclone.

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Anˊti-cy-clon′ic

Adj.

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Anˊti-cy-clon′ic-al-ly

adv.