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Hawan Arctic

Daga Wikipedia, Insakulofidiya ta kyauta.
Hawan Arctic
meteorological phenomenon (en) Fassara
Bayanai
Ƙaramin ɓangare na Rage iska mai nauyi (Haze) da smog (mul) Fassara

Haushi na Arctic shine abin da ke faruwa na haushi mai launin ruwan kasa a cikin yanayi a manyan latitudes a cikin Arctic saboda gurɓataccen iska na mutum.[1] Babban abin da ke rarrabe haze na Arctic shine ikon sinadarai sa don ci gaba a cikin yanayi na tsawon lokaci fiye da sauran gurbatawa. Saboda iyakantaccen dusar ƙanƙara, ruwan sama, ko iska mai rikitarwa don kawar da gurbataccen iska daga iska mai zurfi a cikin bazara, haze na Arctic na iya kasancewa sama da wata ɗaya a cikin yanayin arewa.

  1. Shaw, Glenn E. (December 1995). "The Arctic Haze Phenomenon". Bulletin of the American Meteorological Society. 76 (12): 2403–2413. Bibcode:1995BAMS...76.2403S. doi:10.1175/1520-0477(1995)076<2403:TAHP>2.0.CO;2.