Temperature Advection:
The isentropes show a distinct frontal zone, typical for a Cold Front. There is CA below, within and far in front of the frontal zone which is typical for a Cold Front in Cold Advection, as well as for an Upper Wave.
PVA:
The PVA field shows a maximxum at high levels (300 hPa) above and behind the Upper Wave feature. This is in accodance with the ideal configuration. The distinct PVA maximum within the frontal surface, typical of an ideal case, cannot be seen clearly, but this is quite often the case.
Vertical Motion (Omega):
The field of omega shows strong upward motion in the area of the Cold Front Zone but there is also a backward inclination leading to upward motion at high levels in the area of the Upper Wave. This is in good accordance with the ideal case.
PV:
The isolines of height of PV =2 unit being a measure of the height of the tropopause clearly show a downward inclination behind the Upper Wave till 400 hPa. This is the area with a drop in the WV signal representing the dry, dark stripe. This fits exactly to the ideal configuration of this conceptual model.