Warm air rises due to convection, cooling and condensing into water droplets that form clouds. Moist air forced to rise over hills and mountains also cools and condenses, forming relief rainfall. Frontal rainfall occurs when warm and cold air masses meet, with the warm air forced over cold air cooling and condensing. The main types of clouds are cirrus (high altitude wispy clouds), stratus (middle/low layered clouds), and cumulus (puffy clouds often leading to rain).