An analysis of frontogenesis in numerical simulations of baroclinic waves

Abstract

Using a primitive equation (PE) model, we revisit two canonical flows that were previously studied using a semigeostrophic equation (SG) model. In a previous paper, the authors showed that the PE and the SG models can have significantly different versions of the large-scale dyamics - here they report on the implications of this difference for frontogenesis. The program for the study of frontogenesis developed by B.J. Hoskins and collaborators is followed to show how, in the PE version of the canonical cases, the surface warm front develops before the cold front, and why the upper-level front is a long, nearly continuous feature going from ridge to trough. -from Authors