摘要:Considering the significance of methanesulfonate (MSA) in the sulfur cycle and
global climate, we analyzed MSA and other ionic species in snow from the coastal
Larsemann Hills, East Antarctica. MSA concentrations recorded were high (0.58 ± 0.7 µM) with ice-cap regions showing significantly higher concentrations (df = 10, p < 0.001) than
ice-free regions. High nutrient concentration in ice-cap snow appears to have favored algal growth
(7.6 × 102 cells l − 1) with subsequent production of brominated compounds. The consequent elevated
Br − (3.2 ± 2.2 µM) in the ice-cap region could result in the release of Br atoms through photoactivated reactions
on aerosols and the snow surface. Activated Br atoms in the atmosphere could react with
ozone leading to BrO enhancement with subsequent dimethylsulfide (DMS) oxidation and
production of sulfur aerosols. Since BrO based DMS oxidation is much faster than the
OH/NO3 pathway,
elevated Br − in ice-cap snow could contribute more than ice-free sites towards formation of cloud
condensation nuclei at the expense of ozone.