Isotachs 300 hPa:
There is a long line of a jet stream comprising several maxima, from the rear of the Cold Front to the leading edge of the Warm Front. This is the typical configuration for this conceptual model.
Shear Vorticity 300 hPa:
The field shows a very typical distribution. The zeroline of shear vorticity which represents the jet axis is parallel to the leading edge of the cloud band; the maximum along the cyclonic side identifies a jet atreak.
TFP:
The maximum line of the TFP is very close to the rear edge of the Warm Front cloud band, as expected in the ideal case.
Equivalent Thickness:
There is a distinct gradient of thickness within the Warm Front cloud band. A configuration which is typical for this conceptual model.
Temperature Advection 700 hPa:
The main characteristic of the field of TA in this case is the pronounced WA within the Warm Front cloud band and the CA in the Cold Front behind. This is very typical for the conceptual model of a Warm Front.