Relative Humidity:
The isentropes in this case show a very well developed frontal zone. This is typical even for an area of Front Decay; the
cloud dissolution depends on other parameters. One of them is humidity which shows a protrusion of dry air downward in the
frontal surface. This is very typical.
Temperature Advection:
Also typical for the Conceptual Model of Front Decay is extended CA in the whole area of the frontal surface, as well as in front and behind.
Divergence:
This parameter shows the typical situation for Front Decay: there is mainly divergence within the frontal surface.
Vertical Motion (Omega):
The field of vertical motion corresponds to all the other fields and shows extended sinking within the frontal surface. A
typical configuration of this Conceptual Model.