In principle, if no outside temperature change affects this area (e.g., a warm air mass), the raised albedo and lower temperature would maintain the current snow and invite further snowfall, deepening the snow–temperature feedback.
ɪn pɹˈɪnsɪpəl, ɪf nˈoʊ aʊtsˈaɪd tˈɛmpɹɪtʃɚ tʃˈeɪndʒ ɐfˈɛkts ðɪs ˈɛɹiə ˈiː.dʒˈiː., ɐ wˈɔːɹm ˈɛɹ mˈæs, ðə ɹˈeɪzd ælbˈiːdoʊ ænd lˈoʊɚ tˈɛmpɹɪtʃɚ wʊd meɪntˈeɪn ðə kˈɜːɹənt snˈoʊ ænd ɪnvˈaɪt fˈɜːðɚ snˈoʊfɔːl, dˈiːpənɪŋ ðə snˈoʊ tˈɛmpɹɪtʃɚ fˈiːdbæk.