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Methyl iodine over oceans from the Arctic Ocean to the maritime Antarctic

机译:从北冰洋到南极海洋的甲基碘

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Studies about methyl iodide (CH3I), an important atmospheric iodine species over oceans, had been conducted in some maritime regions, but the understanding of the spatial distribution of CH3I on a global scale is still limited. In this study, we reports atmospheric CH3I over oceans during the Chinese Arctic and Antarctic Research Expeditions. CH3I varied considerably with the range of 0.17 to 2.9 pptv with absent of ship emission. The concentration of CH3I generally decreased with increasing latitudes, except for higher levels in the middle latitudes of the Northern Hemisphere than in the low latitudes. For sea areas, the Norwegian Sea had the highest CH3I concentrations with a median of 0.91 pptv, while the Central Arctic Ocean had the lowest concentrations with all values below 0.5 pptv. CH3I concentration over oceans was affected by many parameters, including sea surface temperature, salinity, dissolved organic carbon, biogenic emissions and input from continents, with distinctive dominant factor in different regions, indicating complex biogeochemical processes of CH3I on a global scale.
机译:在一些海域已经对甲基碘(CH3I)(一种重要的海洋上空碘物种)进行了研究,但对CH3I在全球范围内的空间分布的理解仍然有限。在这项研究中,我们报告了中国北极和南极研究考察期间海洋上空的CH3I。在没有船舶排放的情况下,CH3I变化很大,范围为0.17至2.9 pptv。 CH3I的浓度通常随纬度的增加而降低,除了北半球中纬度的水平高于低纬度以外。在海域,挪威海的CH3I浓度最高,中位数为0.91 pptv,而北冰洋中部的CH3I浓度最低,所有值均低于0.5 pptv。海洋中CH3I的浓度受许多参数的影响,包括海面温度,盐度,溶解的有机碳,生物成因排放和各大洲的输入,在不同区域具有明显的主导因素,表明CH3I在全球范围内复杂的生物地球化学过程。

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