Ice–albedo feedback is a positive feedback climate process where a change in the area of ice caps, glaciers, and sea ice alters the albedo and surface temperature of a planet.
ˈaɪs ælbˈiːdoʊ fˈiːdbæk ɪz ɐ pˈɑːzᵻtˌɪv fˈiːdbæk klˈaɪmət pɹˈɑːsɛs wˌɛɹ ɐ tʃˈeɪndʒ ɪnðɪ ˈɛɹiə ʌv ˈaɪs kˈæps, ɡlˈeɪʃɚz, ænd sˈiː ˈaɪs ˈɔltɚz ðɪ ælbˈiːdoʊ ænd sˈɜːfɪs tˈɛmpɹɪtʃɚɹ əvə plˈænɪt.