Considerations of moist air and cloud theories typically involve various temperatures, such as equivalent potential temperature, wet-bulb and virtual temperatures.
kənsˌɪdɚɹˈeɪʃənz ʌv mˈɔɪst ˈɛɹ ænd klˈaʊd θˈiəɹiz tˈɪpɪkli ɪnvˈɑːlv vˈɛɹiəs tˈɛmpɹɪtʃɚz, sˈʌtʃ ɐz ɪkwˈɪvələnt pətˈɛnʃəl tˈɛmpɹɪtʃɚ, wˈɛtbˈʌlb ænd vˈɜːtʃuːəl tˈɛmpɹɪtʃɚz.