6. now let's follow the imaginary dynamics of an evolving environment starting with the conditions in the previous problem. assume that the amount of water vapor in the environment (e-the vapor pressure) changes such that the environment is saturated with respect to liquid water. also assume temperature remains equal to the previous problem, and constant throughout. a. what is the in-cloud rh in this environment? b. calculate the ambient rh, within this new environment c. will liquid droplet grow. shrink, or remain the same in this environment? d. will ice particles grow. shrink, or remain the same in this environment? why can we ignore the limitations of the curvature effect on droplet growth in this problem?