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首页> 外文期刊>Advances in space research >Cosmogenic isotope ~7Be: A case study of depositional processes in Rio de Janeiro in 2008-2009
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Cosmogenic isotope ~7Be: A case study of depositional processes in Rio de Janeiro in 2008-2009

机译:宇宙成因同位素〜7Be:以里约热内卢2008-2009年的沉积过程为例

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摘要

We present here an investigation of the depositional processes of ~7Be-carrying aerosols in the troposphere through an analysis of the isotope concentration variability measured at Rio de Janeiro (Brazil) during 2008 and 2009, with weekly resolution. By adopting a simplified description of the equilibrium scenario in the troposphere and combining our isotopic data with regional meteorological parameters and numerical CRAC:Be7 model of cosmogenic production, it was possible to quantitatively reproduce the observed seasonal variability and estimate the typical ~7Be-aerosols residence time in the lower troposphere (t_r ~ 1 day) as well as the washout coefficient for each season (wet: A = 0.029; and dry: A = 0.023 h~(-1)). These results allowed us to discuss the origin of the seasonal patterns of ~7Be concentrations, indicating that the wet deposition modulation, caused by changes in the regional weather condition, is the most important forcing in both seasons. Even an anomaly in isotopic short-term measured variability can be explained when a detailed air-mass dynamic is considered. Our results indicate that anomalous events of tropospheric dynamic, such as occurrence of strong downward air flux, imprint information about air masses 3-D movement in the near-ground air ~7Be data, making ~7Be a useful tracer of its peculiar dynamics at local and synoptic scales in the troposphere. This study, limited to a single location and one year time interval, illustrates the potential of the method. A more detailed general study is planned for the future.
机译:我们通过对2008年和2009年在巴西里约热内卢测量的同位素浓度变异性进行分析,以周分辨率的方式,对这里对流层中〜7Be气溶胶的沉积过程进行了调查。通过对流层中平衡情景的简化描述,并将我们的同位素数据与区域气象参数和数值CRAC:Be7的宇宙成因生产相结合,可以定量地再现观测到的季节性变化并估算典型的〜7Be-气溶胶驻留对流层下部的时间(t_r〜1天)以及每个季节的冲刷系数(湿:A = 0.029;干:A = 0.023 h〜(-1))。这些结果使我们能够讨论〜7Be浓度的季节模式的起源,表明由区域天气状况的变化引起的湿沉降调节是两个季节中最重要的强迫。当考虑详细的空气动力学时,甚至可以解释同位素短期测量的变异性异常。我们的结果表明,对流层动力学的异常事件,例如强向下气流的发生,有关近地空气中空气质量3-D运动的印迹信息〜7Be数据,使〜7Be成为其局部局部动力学的有用示踪剂和对流层的天气尺度。这项研究仅限于单个地点和一年的时间间隔,说明了该方法的潜力。计划在将来进行更详细的一般研究。

著录项

  • 来源
    《Advances in space research》 |2011年第5期|p.811-818|共8页
  • 作者单位

    Department of Physics, University of Oulu, 90014 Oulu, Finland,IP&D, University of Vale do Paraiba, 12244-000, Sao Jose dos Campos, Brazil,National Institute for Space Research, 12227-010, Sao Jose dos Campos, Brazil;

    Sodankylae Geophysical Observatory (Oulu Unit), University of Oulu, 90014 Oulu, Finland;

    University of Rio de Janeiro State, 20550-013, Rio de Janeiro, Brazil;

    National Institute for Space Research, 12227-010, Sao Jose dos Campos, Brazil;

    University of Rio de Janeiro State, 20550-013, Rio de Janeiro, Brazil;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    cosmogenic isotopes; atmospheric transport; tropospheric depositional processes;

    机译:宇宙成因同位素大气运输;对流层沉积过程;

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