The intensity of albedo temperature effects depends on the amount of albedo and the level of local insolation (solar irradiance); high albedo areas in the Arctic and Antarctic regions are cold due to low insolation, whereas areas such as the Sahara Desert, which also have a relatively high albedo, will be hotter due to high insolation.
ðɪ ɪntˈɛnsᵻɾi ʌv ælbˈiːdoʊ tˈɛmpɹɪtʃɚɹ ɪfˈɛkts dᵻpˈɛndz ɔnðɪ ɐmˈaʊnt ʌv ælbˈiːdoʊ ænd ðə lˈɛvəl ʌv lˈoʊkəl ˌɪnsəlˈeɪʃən sˈoʊlɚɹ ˈɪɹeɪdˌiəns; hˈaɪ ælbˈiːdoʊ ˈɛɹiəz ɪnðɪ ˈɑːɹktɪk ænd æntˈɑːɹktɪk ɹˈiːdʒənz ɑːɹ kˈoʊld dˈuː tə lˈoʊ ˌɪnsəlˈeɪʃən, wˈɛɹæz ˈɛɹiəz sˈʌtʃ ɐz ðə sɐhˈæɹə dˈɛzɚt, wˌɪtʃ ˈɔːlsoʊ hæv ɐ ɹˈɛlətˌɪvli hˈaɪ ælbˈiːdoʊ, wɪl biː hˈɑːɾɚ dˈuː tə hˈaɪ ˌɪnsəlˈeɪʃən.