Which statement is true about updrafts in the dissipating stage of a thunderstorm?

In the dissipating stage of a thunderstorm, updrafts cease entirely as the storm begins to lose its energy and intensity. During this stage, the processes that originally fueled the thunderstorm, such as warm, moist air rising to create updrafts, are diminished. As the storm weakens, the cooling effect of the precipitation falling within the storm contributes to a lack of rising air. This results in the dissipation of the updrafts, signaling the storm is moving towards its end. Consequently, the storm's characteristics change as it no longer can sustain the powerful updrafts necessary for maintaining its structure and severity.