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7Be aerosols in the Arctic atmosphere - modelling of air mass trajectories

机译: 7 成为北极大气中的气溶胶-空气轨迹的建模

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The activity size distributions of the natural radionuclide tracer 7Be in different inhalable fractions (<0.39 µm, 0.391–0.69 µm, 0.69–1.3 µm, 1.3–2.1 µm, 2.1–4.2 µm, 4.2–10.2 µm and >10.2 µm) were determined in the boreal atmosphere in the Arctic Research Centre of the Finnish Meteorological Institute (FMI) at Sodankylä, Finland (67°22′ N, 26°38′ E, 180m asl). The activity median aerodynamic diameter (AMAD) ranged from 0.54 µm to 1.05 µm. More than 75% of the 7Be activity was found to be associated with particles smaller than 1.3 µm. An anticorrelation was observed between the AMAD values and 7Be activities. The observed correlation between the AMAD values and RH% can be due to the intense condensation process during high RH% conditions resulting in increased particle sizes. But this associated with possibly higher scavenging rates of aerosols does not necessarily alone explain the anticorrelation between the AMAD and the 7Be activities. The air mass origin associated with synoptic scale weather phenomena may contribute to that too. To study this an analysis of air mass back-trajectories was performed.
机译:天然放射性核素示踪剂 7 Be的活动大小分布在不同的可吸入部分(<0.39 µm,0.391–0.69 µm,0.69–1.3 µm,1.3–2.1 µm,2.1–4.2 µm,4.2–10.2是在芬兰Sodankylä的芬兰气象研究所(FMI)北极研究中心的北极大气中测定的微米(> 10.2 µm)(67°22'N,26°38'E,180m asl)。活动的空气动力学中值直径(AMAD)为0.54 µm至1.05 µm。发现超过75%的 7 Be活性与小于1.3 µm的颗粒有关。在AMAD值和 7 Be活性之间观察到反相关。观察到的AMAD值和RH%之间的相关性可能是由于在高RH%条件下剧烈的冷凝过程导致了粒径的增加。但这可能与更高的气溶胶清除率有关,并不一定单独解释了AMAD与 7 Be活性之间的反相关性。与天气尺度天气现象有关的空气质量起因也可能是这一原因。为了研究这一点,进行了空气质量后退轨迹的分析。

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