A review of the structure and dynamics of upper-level frontal zones
The development of structural models of upper-level frontal systems from the application of upper-air data to analyses utilizing radiosonde and aircraft observations is reviewed. The effects of turbulent processes and baroclinic waves on frontal structures and dynamics are examined. The use of the Sawyer-Eliassen (1956) equation for calculating the geostrophic, vertical circulations assosicated with frontal zones is described. The formation of upper-level fronts in two-dimensional flows and in three-dimensional baroclinic waves is studied and examples are provided. Future observational, diagnostic, and theoretical investigations on upper-level frontal zones are discussed.