noun
: the half of the nearly circular area of a cyclonic storm in which the velocity of rotation is added to the velocity of translation and in which a vessel tends to be drawn into the path of the storm center
noun
: the half of the nearly circular area of a cyclonic storm in which the velocity of rotation is added to the velocity of translation and in which a vessel tends to be drawn into the path of the storm center
Webster's New International English Dictionary. Новый международный словарь английского языка Webster. 2012