bɪkˈʌz mˈɛni kˈeɪvz hæv sˈiːzənəliɹᵻvˈɜːsɪŋ dɹˈæfts, ðə kˌɔːɹɪspˈɑːndɪŋ wˈɔːɹmɪŋ ʌvðə kˈeɪv θɹuː kɑːndɛnsˈeɪʃən ɪn sˈʌmɚ mˈeɪ əkˈɜːɹ æɾə dˈɪfɹənt loʊkˈeɪʃən wɪðˌɪn ðə kˈeɪv, bˌʌt ɪn ˌɛni ᵻvˈɛnt ɐ mˈɔɪstʃɚsˈætʃɚɹˌeɪɾᵻd kˈeɪv ɛnvˈaɪɹənmənt ɪz lˈaɪkli tʊ ɛkspˈiəɹɪəns mˈʌtʃ mˈoːɹ ɪvˈæpɹətˌɪv kˈuːlɪŋ ðɐn kəndˈɛnsətˌɪv wˈɔːɹmɪŋ.
Because many caves have seasonally-reversing draughts, the corresponding warming of the cave through condensation in summer may occur at a different location within the cave, but in any event a moisture-saturated cave environment is likely to experience much more evaporative cooling than condensative warming.