Ukuba i-polar aurora ibonwa ukusukela kwinkungu yexesha, kubonakala ngathi amafu imvulophu Zibonakala ekupheleni kwenkulungwane ye-XIX. Singalindela ukubabona ngakumbi nangakumbi rhoqo, ukuba stratospheric umphunga wamanzi iyaqhubeka isanda.
Ukuxinaniswa kabini kwe ikharbon diokside emoyeni iya kunyuka, iyodwa, iqondo lobushushu behlabathi eliyi-1,2ºC. Nangona kunjalo, imozulu sisayensi eguqukayo. Inkqubo ye- ulwandle, imiphezulu yelizwekazi kunye namanqanaba ohlukeneyo omoya asabela koku ukulungiswa, evumela iimpendulo ezinokuphakamisa lobushushu umndilili wehlabathi ukusuka kwi-2 ukuya kwi-4,5ºC.
Ukuphendula mozulu ngokunxulumene nokwanda kokukhutshwa kwegesi ekrwada kuyaziwa ngabo bonke, kodwa ukungaqiniseki ziqhubeka ngokunxulumene nokuphendula kwamafu i-aerosol iyatyabeka, umzekelo.
Umzekelo we uqikelelo Imozulu zama ukulinganisa ngokuchanekileyo ngokuchanekileyo zonke ezi zinto ukuphendula elawula ukuvela kwemozulu. Iqela lophando laseMelika lifunde ngokweenkcukacha enye yazo, ingahoywa ixesha elide luluntu: ibandakanya stratosphere, Eziza kuphendula kukwanda kwe- lobushushu zomoya kumphezulu womhlaba, ukwandisa inani lawo umphunga zamanzi.
El umphunga wamanzi yirhasi yegreenhouse enamandla, kwaye esi sixhobo sinegalelo ekunyukeni kwe ubushushu bomoya.
Iinkcukacha ezithe xaxe - Umngxunya kumaleko weozone ongezantsi kweepali