Process of weakening or terminating of a cyclonic circulation in the atmosphere; the opposite of cyclogenesis.
(from the article `climate`) ...followed by further storm intensification. The separation of the cyclone from the warm air toward the Equator, however, eventually leads to the ...
process of weakening or terminating of a cyclonic circulation in the atmosphere; the opposite of cyclogenesis .
the weakening or extinction of a cyclone. Cf. cyclogenesis.