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H<jats:sub>2<\/jats:sub>O<jats:sub>2<\/jats:sub> smatra se boljim indikatorom za atmosferski oksidacijski kapacitet od ozona. U atmosferi mo\u017ee biti prisutan u plinovitoj i teku\u0107oj fazi te pokazuje tipi\u010dne dnevne i sezonske varijacije. Me\u0111utim, zbog skupe i slo\u017eene opreme, mjerenja H<jats:sub>2<\/jats:sub>O<jats:sub>2<\/jats:sub> su rijetka i ograni\u010dena na samo nekoliko mjesta u svijetu. Mjerenja u slojevima leda na Grenlandu pokazala su da koncentracije H<jats:sub>2<\/jats:sub>O<jats:sub>2<\/jats:sub> rastu posljednjih 200 godina. Zna\u010dajan porast primije\u0107en je upravo posljednjih dvaju desetlje\u0107a, a procjene pokazuju da \u0107e i dalje rasti zbog smanjene emisije sumporova dioksida. 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