Height of PV=1

1st July 2004: 06UTC
The high gradient of the isolines manifest the frontal area. Two parts show a deeper downward intrusion of stratospheric air.

1). Behind the frontal system over the Northsea.

2). Over northeast Germany and Poland, which is an area where a double structure in the frontal system can be observed. Although from the field of temperature advection this part shows up as Warm front sector this is not supported by the appearance of cloudiness in satellite images nor by the height of PV=1 discussed here. The latter would rather diagnose an older cold front system