Summary
The separation of potential temperature and equivalent-potential temperature patterns at cold fronts with pre-frontal foehn is explained by means of conceptual considerations and discussed with reference to observations and numerical simulations. It is shown that foehn increases the potential temperature north of the Alps but does not necessarily affect the equivalent-potential temperature. As a consequence potential temperature and equivalent-potential temperature may form different structures and generate zones of large gradients at different locations even if no diabatic heat conversions are present.
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Heimann, D. Potential and equivalent-potential temperature patterns at cold fronts with pre-frontal foehn. Meteorl. Atmos. Phys. 48, 165–171 (1992). https://doi.org/10.1007/BF01029565
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DOI: https://doi.org/10.1007/BF01029565