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Spatial Distribution of Methanesulphonic Acid in the Arctic Aerosol Collected during the Chinese Arctic Research Expedition

机译:中国北极研究考察期间收集的北极气溶胶中甲磺酸的空间分布

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Methanesulphonic acid (MSA, mainly derived from marine biogenic emissions) has been frequently used to estimate the marine biogenic contribution. However, there are few reports on MSA over the Arctic Ocean, especially the central Arctic Ocean. Here, we analyzed MSA in aerosol samples collected over the ocean and seas during the Chinese Arctic Research Expedition (CHINARE 2012) using ion chromatography. The aerosol MSA concentrations over the Arctic Ocean varied considerably and ranged from non-detectable (ND) to 229 ng/m3, with an average of 27 ± 54 ng/m3 (median: 10 ng/m3). We found the distribution of aerosol MSA exhibited an obvious regional variation, which was affected by biotic and abiotic factors. High values were generally observed in the Norwegian Sea; this phenomenon was attributed to high rates of phytoplankton primary productivity and dimethylsulfide (DMS) fluxes in this region. Concentrations over the pack ice region in the central Arctic Ocean were generally lower than over the open waters at the ice edge in the Chukchi Sea. This difference was the mainly caused by sea ice. In addition, we found that higher MSA concentrations were associated with warmer sea surface temperature (SST).
机译:甲磺酸(MSA,主要来自海洋生物排放物)经常被用来估算海洋生物的贡献。但是,关于北冰洋,特别是北冰洋中部的MSA的报道很少。在这里,我们使用离子色谱法分析了中国北极研究考察队(CHINARE 2012)在海洋中收集的气溶胶样品中的MSA。北冰洋的气溶胶MSA浓度变化很大,范围从不可检测(ND)到229 ng / m 3 ,平均为27±54 ng / m 3 (中位数:10 ng / m 3 )。我们发现气溶胶MSA的分布表现出明显的区域变化,受生物和非生物因素的影响。在挪威海普遍观察到较高的价值;这种现象归因于该地区浮游植物的初级生产力和二甲基硫(DMS)通量较高。北冰洋中部浮冰区的浓度通常低于楚科奇海冰缘的开放水域的浓度。这种差异主要是由海冰引起的。此外,我们发现较高的MSA浓度与海表温度(SST)升高有关。

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