| Summary: | The development of several major cases of persistent negative height anomalies over the extratropical central North Pacific and eastern North Atlantic regions was investigated. These events were manifested at the surface by the development of large-scale cyclonic circulations and, at upper levels, by the formation of anomalously intense zonal jets. The data for the analyses were obtained from the twice-daily NMC final analyses of Northern Hemisphere sea-level pressure as well as geopotential heights, winds, and temperatures at all standard levels from 1000 mb to 100 mb for the fourteen winter seasons from years 1963-1964 through 1976-1977. The results indicate that, in many cases of cyclogenesis, baroclinic processes are likely to play an important role in the initial developments. At later stages, barotropic processes also provide significant contributions and play a role in the maintenance of the anomalies once they are established.
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