Height Contours 500 hPa:
This is a very typical example of a Baroclinic Boundary at the western part of an intensive upper level trough. Although
there is a continuous cloud band, it is located on the "wrong" side of the trough.
TFP:
This case shows a situation where the Baroclinic Boundary is accompanied by a well developed Thermal Front Parameter, which
indicates that there is a change in the temperature gradient similar to a front. However, from the location in the synoptic
scale field it is not an active front.
Equivalent Thickness:
Although thickness shows a typical configuration where the cloudiness of the Baroclinic Boundary is at the warm side of the
zone of high gradients, the cloud is on the "wrong" side of the thickness trough.
Temperature Advection 700 hPa:
Temperature Advection does not show a continuous zero line in the area of the cloud of the Baroclinic Boundary, but centres
of warm and cold advection. As there is no typical configuration of temperature advection in connection with the cloud
band of a Baroclininc Boundary, this is a special behaviour of this case.