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.
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.