Θw:
The most important feature is the unstable air mass up to 600 hPa in the area of the developing CBs.
Relative Humidity:
As in the ideal case, there is moist in lower layers and relative dry air in the higher layers.
Temperature Advection:
The vertical distribution of Temperature Advection in the centre of the area of the Cumulonimbus Cluster shows some WA in the lower layers and hardly any TA in higher layers. In the east part of the area the CA is a negative feedback parameter and can stop the convection.
Divergence:
The convergence in the lower layers is not as clear as in the ideal case. In the vertical the distribution of the divergence and convergence shows no uniform structure.