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

机译:7 是北极气氛的气溶胶 - 空气质量轨迹的建模

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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的活动尺寸分布 7 具有不同可吸入级分(<0.39μm,0.391-0.69μm,0.69-1.3μm,1.3-2.1μm,2.1-4.2μm,4.2-10.2 μm和>10.2μm)在芬兰芬兰芬兰气象研究所(FMI)的北极研究中心(FMI)的北极研究中心(FMI)的北极大气中测定(67°22'n,26°38'e,180m ASL)。活动中值的空气动力学直径(AMAD)范围为0.54μm至1.05μm。发现超过75%的 7 是活性,与小于1.3μm的颗粒相关。在AMAD值和 7 是活动之间观察到一个反相。所观察到的AMAD值和RH%之间的相关性可以是由于在高压铑条件下的强凝结过程导致导致粒度增加。但是,这种与可能更高的气溶胶清除率相关的这种速率并不一定单独解释AMAD和 7 的反作用。与揭示尺度天气现象相关的空气质量可能会有助于这一点。为了研究这一点,进行了对空气质量背轨迹的分析。

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