An example of a convective cloud is the

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Convective clouds are formed due to convection, where warm air rises and cools as it ascends, forming clouds. Cumulus clouds are classic examples of convective clouds, as they are formed due to rising air currents. The other options are not convective clouds - nimbostratus clouds are formed due to a large swath of moist air being lifted, cirrocumulus clouds are high-level clouds formed due to the mixing of two air masses, and altostratus clouds are mid-level clouds formed due to warm air moving up and over a cold front.

An Example of a Convective Cloud Is the