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Variability of atmospheric dimethylsulphide over the southern Indian Ocean due to changes in ultraviolet radiation

机译:紫外线变化引起印度洋南部大气中二甲基硫的变化

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摘要

[1] Dimethylsulphide (DMS) is a climatically important component of global biogeochemical cycles, through its role in the sulphur cycle. Changes in ultraviolet radiation (UV) exhibit both positive and negative forcings on the dynamics of production and turnover of DMS and its precursor dimethylsulphoniopropionate (DMSP). In this study we investigate the net forcing of UV on atmospheric DMS. The work is based on a 10-year record of observed DMS at Amsterdam Island in the southern Indian Ocean, and satellite-based retrievals of surface UV and photosynthetically active radiation (PAR). The results show an inverse relationship between UV radiation and atmospheric DMS associated with extreme changes (defined as the greatest 5%) in daily UV, independent of changes in wind speed, sea surface temperature, and PAR.
机译:[1]二甲基硫化物(DMS)通过其在硫循环中的作用,是全球生物地球化学循环的气候重要组成部分。紫外线(UV)的变化对DMS及其前体二甲基磺酸丙二酸酯(DMSP)的生产和周转动力学表现出正向和负向强迫。在这项研究中,我们研究了紫外线在大气DMS上的净强迫。这项工作是基于在印度洋南部的阿姆斯特丹岛观测到的DMS的十年记录,以及基于卫星的表面紫外线和光合有效辐射(PAR)的检索。结果表明,紫外线辐射与大气DMS之间存在反比关系,而后者与每日紫外线的极端变化(定义为最大5%)相关,而与风速,海面温度和PAR的变化无关。

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