Relative Humidity:
The isentropes show a zone of high gradients with a very flat inclination. This speaks for the fact, that the low cloud
which can be seen to the west has also some frontal character. The rel. humidity shows high values at low and at high
levels. Especially the latter represents the high cloud of the Detached Warm Front. So there is a very typical distribution
of this parameter for the conceptual model of a Detached Warm Front.
Temperature Advection:
There is pronounced WA in the frontal zone and in the area of the cloud of the Detached Warm Front. This corresponds very
well with the ideal ideas of this conceptual model.
Divergence:
The field of divergence shows two maxima of convergence in the frontal zone which are upward inclined within the frontal
zone. Divergence can be found above. This is very typical for a Warm Front area and supports the activity of the front.
Vertical Motion (Omega):
Vertical motion is rather weak. The values show only very weak ascent in the frontal zone; no separate maxima can
be observed. This - somewhat - contradicts the activity of this Detached Warm Front case which is observed in the cloud field as well as in other parameters, such as convergence.
Isotachs:
There is a pronounced jet streak with its maximum at the western (the leading) border of the cloud band. This is very
typical for the conceptual model of a Detached Warm Front.