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The central dense overcast, or CDO, of a tropical cyclone or strong subtropical cyclone is the large central area of thunderstorms surrounding its circulation center, caused by the formation of its eye wall. It can be round, angular, oval, or irregular in shape. This feature appears in tropical cyclones of tropical storm or hurricane strength.

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rdfs:comment	The central dense overcast, or CDO, of a tropical cyclone or strong subtropical cyclone is the large central area of thunderstorms surrounding its circulation center, caused by the formation of its eye wall. It can be round, angular, oval, or irregular in shape. This feature appears in tropical cyclones of tropical storm or hurricane strength.
rdfs:seeAlso	dbpedia:Dvorak_technique
foaf:depiction
thumbnail	http://commons.wikimedia.org/wiki/Special:FilePath/Alberto_May_19_2012_1610Z_(cropped).jpg?width=300

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