What type of clouds are typically associated with the passage of a cold front?

Cumulonimbus clouds are indeed typically associated with the passage of a cold front due to their characteristics related to rapidly rising air and severe weather conditions. When a cold front moves through an area, the colder, denser air forces warmer, moist air to rise quickly. This rapid ascent of the warm air can lead to the development of cumulonimbus clouds, which are characterized by their towering structure and can produce heavy rainfall, thunderstorms, and sometimes severe weather phenomena such as hail or tornadoes.

These clouds form as a result of significant vertical development, which is a hallmark of cold fronts. As the moist air rises, it cools and condenses, forming the thick, towering cumulonimbus clouds that we often associate with stormy weather. This is in contrast to the other types of clouds mentioned, which are less commonly associated with the dramatic weather changes that accompany cold fronts.