The Convergence Cloudiness CM represents a quasi-frontal situation, in effect, attached to the end of an Occlusion. Therefore weather events are frontal in character.

Parameter	Description
Precipitation	Widespread precipitation in the form of rain or snowfall, in some cases it can be more than from Occlusion cloudiness. Convective features are unlikely.
Temperature	Rises weakly after Convergence Cloudiness
Wind (incl. gusts)	Surface winds weak at the transition zone where the cloudiness joins the Occlusion
Other relevant information	None