In addition, the contributions of CHON molecules in unique molecular components showed an increasing trend of 21.56% in fresh snow, 39.87% in fine firn, 42.67% in coarse firn, and 43.60% in granular ice, which suggested that the snow metamorphism could alter the component of DOM.
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Biochemical evolution of dissolved organic matter during snow metamorphism across the ablation season for a glacier on the central Tibetan Plateau.
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