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CYCLOLYSIS

Cyclolysis

Dissipation of a cyclone

Cyclolysis is a process in which a cyclonic circulation weakens and deteriorates. Cyclolysis is the opposite of cyclogenesis. Extratropical cyclones usually

Cyclolysis

Cyclogenesis

Development or strengthening of cyclonic circulation in the atmosphere

high-pressure areas, is anticyclogenesis. The opposite of cyclogenesis is cyclolysis. There are four main scales, or sizes of systems, dealt with in meteorology:

Cyclogenesis

Low-pressure area

Area with air pressures lower than adjacent areas

low-pressure areas, within the atmosphere. Cyclogenesis is the opposite of cyclolysis, and has an anticyclonic (high-pressure system) equivalent which deals

Low-pressure area

Low-pressure_area

Cyclone

Large scale rotating air mass

develop from environments of high instability and low vertical wind shear. Cyclolysis is the opposite of cyclogenesis, and is the high-pressure system equivalent

Cyclone

Extratropical cyclone

Type of cyclone

Weather portal Nor'easter Sudestada Cyclogenesis Explosive cyclogenesis Cyclolysis Late December 1999 European storms DeCaria (2005-12-07). "ESCI 241 – Meteorology;

Extratropical cyclone

Extratropical_cyclone

Eady model

Mathematical model of instability in the atmosphere

induced, decreasing potential vorticity and pressure anomalies and yielding cyclolysis. Making Fourier decompositions on the linearized Eady model equations

Eady model

Eady_model

Brown ocean effect

Weather phenomenon

status well inland over Western Australia due to the brown ocean effect. Cyclolysis Unusual areas of tropical cyclone formation Jeff Masters; Bob Henson (15

Brown ocean effect