Temperature Advection:
The isentropes in this case show only a very indistinct and unstable Cold Front character by far not as developed as
described in the ideal situation. But TA contains the transition from WA in front to CA behind the frontal surface very
well. The extended area of WA in front of the CAD cloudiness seems to be connected to the Occlusion of the main frontal
system.
PVA:
There is a huge and intensive PVA maximum superimposed on the cloudiness of the CAD. This is in good agreement with the
ideal situation.
