There is indication of upward motion in the entire region of the cross-section, but the intensity is not very strong.
Isotachs do not show any prominent maximum, which means that the cross-section does not cut the jet stream, but it flows either parallel to it or in the region where the wind is not very strong.
Vorticity field does not show any prominent features. Weak negative (anticyclonic) vorticity preveals in this cross section.
Warm advection region extends throughout the whole cross-section.
Vorticity advection does not show any prominent maxima. Weak maximum of negative vorticity advection is found in the upper troposphere in the left-hand side of the cross-section.