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Below-cloud scavenging of size-segregated aerosols and its effect on rainwater acidity and nutrient deposition: A long-term (2009-2018) and real-time observation over eastern Himalaya

机译:喜马拉雅东部东部地区(2009-2018年)的长期(2009-2018年)实时观测:云团清除后的尺寸分离气溶胶及其对雨水酸度和养分沉积的影响

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摘要

The major removal pathway of atmospheric aerosols is the below cloud scavenging. The present study is the first-ever in the world, where long-term(2009-2018) as well as real-time observations on the below-cloud scavenging of ultrafine (0.4 mu m), superfine (0.4-1.0 mu m) and coarse mode (1 mu m) aerosols have been made. The study was conducted with 919 rain events over a high altitude Himalayan station (27.01 degrees N, 88.15 degrees E, 2200 m amsl) in India. The other factors were normalized in order to investigate the "rain only" effect and therefore 919 rain events were screened and finally 165 events were studied. We determined threshold values of the rain rate (and duration) above which aerosols are scavenged in very high proportion (75%) irrespective of the duration (and rain rate). These threshold values decrease as the aerosol size increases. For example, threshold rain rate decreases from similar to 17 mm h(-1) to similar to 8 mm h(-1) as the aerosol size increases from ultrafine to coarse mode. We also showed that how the rainwater acidity and the deposition flux of major inorganic nutrients (NH4+ + NO3- + SO42-) vary with the rain rate and duration. We observed that the rains either 12 mm h(-1) or 80 min are all acidic. Maximum nutrients were accumulated in the ultrafine aerosols and hence the spectrum of the deposition flux of the nutrients (with rain rate and duration) was similar to the scavenging spectrum of ultrafine aerosol. Such long-term database enables us to quantitatively predict the aerosol scavenging, acid rains and nutrient deposition which showed excellent agreement with the observed results. Such quantitative prediction would in turn help the researchers to predict the rain-induced changes in air quality as well as any bio-geo chemical parameter. The present study bears paramount importance in Himalayan context as well as any ecologically-rich regions. (C) 2019 Elsevier B.V. All rights reserved.
机译:大气气溶胶的主要清除途径是清除云层以下。本研究是世界上第一个对超细颗粒物(<0.4微米),超细颗粒物(0.4-1.0微米)进行云层长期清除(2009-2018年)的实时观测资料)和粗模式(> 1μm)的气雾剂。该研究在印度喜马拉雅高海拔站(北纬27.01度,东经88.15度,2200 m amsl)上进行了919次降雨事件。为了研究“仅降雨”效应,将其他因素归一化,因此筛选了919个降雨事件,最后研究了165个降雨事件。我们确定了降雨率(和持续时间)的阈值,在该阈值之上,无论持续时间(和降雨率)如何,都以很高的比例(> 75%)清除了气溶胶。这些阈值随着气溶胶尺寸的增加而降低。例如,随着气溶胶尺寸从超细模式增加到粗模式,阈值降雨率从相似的17 mm h(-1)降低到相似的8 mm h(-1)。我们还表明,雨水酸度和主要无机养分(NH4 + + NO3- + SO42-)的沉积通量如何随降雨率和持续时间而变化。我们观察到,> 12 mm h(-1)或> 80 min的降雨都是酸性的。在超细气溶胶中积累了最多的养分,因此养分的沉积通量的光谱(随降雨率和持续时间的变化)与超细气溶胶的清除谱相似。这样的长期数据库使我们能够定量地预测气溶胶清除,酸雨和养分沉积,这与观测结果具有极好的一致性。这样的定量预测反过来将有助于研究人员预测降雨引起的空气质量变化以及任何生物地球化学参数。在喜马拉雅地区以及任何生态丰富的地区,本研究都至关重要。 (C)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《The Science of the Total Environment》 |2019年第15期|223-233|共11页
  • 作者单位

    Bose Inst, Environm Sci Sect, P1-12 CIT Scheme 7-M, Kolkata 700054, India;

    Bose Inst, Environm Sci Sect, P1-12 CIT Scheme 7-M, Kolkata 700054, India|Bose Inst, Natl Facil Astroparticle Phys & Space Sci, 16 AJC Bose Rd, Darjeeling 734101, India;

    Bose Inst, Environm Sci Sect, P1-12 CIT Scheme 7-M, Kolkata 700054, India;

    Bose Inst, Environm Sci Sect, P1-12 CIT Scheme 7-M, Kolkata 700054, India;

    Bose Inst, Environm Sci Sect, P1-12 CIT Scheme 7-M, Kolkata 700054, India|Bose Inst, Natl Facil Astroparticle Phys & Space Sci, 16 AJC Bose Rd, Darjeeling 734101, India|Bose Inst, Ctr Astroparticle Phys & Space Sci, Block EN,Sect 5, Kolkata 700091, India;

    Bose Inst, Natl Facil Astroparticle Phys & Space Sci, 16 AJC Bose Rd, Darjeeling 734101, India|Bose Inst, Ctr Astroparticle Phys & Space Sci, Block EN,Sect 5, Kolkata 700091, India;

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

    Below-cloud scavenging; Rainwater acidity; Nutrient deposition; Size-segregated aerosols; Eastern Himalaya;

    机译:清除云层以下;雨水酸度;营养物沉积;按尺寸分离的气溶胶;喜马拉雅东部;

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