TFP:
The location of the TFP in relation to the frontal cloud band corresponds very well to the ideal situation.
Equivalent Thickness:
In the ideal case, a thickness gradient within or close to the rear of the frontal cloud band is to be expected. In this case
however, there is only a very small or almost no gradient. This means at least that it is a far advanced case with very
weak temperature contrasts.
Temperature Advection 700 hPa:
The temperature advection field shows a zeroline behind the rear edge of the frontal cloud band, leading to warm advection
also behind the frontal cloud band. This corresponds to the ideal case, although there are cases with an even more distinct
effect.
Omega:
This case shows rather high values of upward motion, which in an ideal case of a Cold Front in Warm Advection is not
expected.
Relative Humidity:
There are rather low values of relative humidity (< 50%) connected to the cloud band of the Cold Front. Even lower
values can be seen immediately behind (< 20%). This is an indication for dry advection which corresponds well to the
ideal situation of a Cold Front in Warm Advection.