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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Long‐Term Investigation of Aerosol Optical and Radiative Characteristics in a Typical Megacity of Central China During Winter Haze Periods
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Long‐Term Investigation of Aerosol Optical and Radiative Characteristics in a Typical Megacity of Central China During Winter Haze Periods

机译:冬季阴霾时期典型的巨大明显典型巨型气泡光学和辐射特性的长期调查

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摘要

Decadal aerosol characteristics and related radiative effects (ARE) and efficiencies (AREE) at ultraviolet (UV), visible (VIS), near‐infrared (NIR), and shortwave wavelengths were investigated in Wuhan during winter haze periods based on observations from 2007 to 2016. Aerosols changed significantly under haze conditions; the average aerosol optical depth increased from 0.46 to 0.93, and the ?ngstr?m exponent increased from 1.12 to 1.23. Fine‐mode particles became dominant, and their peak radius also increased due to hygroscopic growth. The mean value of the UV single‐scattering albedo increased from 0.846 to 0.873, revealing the emergence of numerous fine‐mode, nonabsorbing aerosols. Backward trajectories suggested that local aerosols were partially affected by transported dust from Northwest China, especially in 2015. The interannual variation of the mean AREE at the top of atmosphere showed a gradually increasing tendency, revealing the enhanced potential cooling capacity of aerosols to the Earth‐atmosphere system over Wuhan. The increase in the AREE fraction at UV and VIS wavelengths, and its decrease at NIR wavelengths, indicated that this phenomenon was due to the increased proportion of fine‐mode scattering components in aerosols. The variation in AREE at top of atmosphere depended mainly on the single‐scattering albedo, while the same variation at the surface depended more on particle sizes. A detailed investigation of aerosols during haze periods can help us to further understand localized climate variations and haze‐inducing mechanisms.
机译:在冬季阴霾期间在2007年的观察期间在武汉在武汉研究了紫外线(UV),可见(VI),近红外(NIR),可见(VI),近红外(NIR)和短波波长的近代气溶胶特性和相关辐射效果(AREE)和效率(AREE)。 2016年。在阴霾条件下,气溶胶显着变化;平均气溶胶光学深度从0.46增加到0.93,αngstrΔM指数从1.12增加到1.23。细模颗粒变得显着,由于吸湿生长,它们的峰半径也增加。 UV单散射玻璃玻璃的平均值从0.846增加到0.873,揭示了许多微型,非吸血剂气溶胶的出现。落后的轨迹表明,局部气溶胶受到来自西北地区的运输粉尘的部分影响,特别是2015年。大气层顶部的平均终际变化表现出逐渐增加的趋势,揭示了气溶胶到地球的增强潜在的冷却能力 - 武汉大气系统。 UV和VIS波长的A1E部分级分的增加及其在NIR波长下的降低,表明这种现象是由于气溶胶中的微型散射组分比例增加。在大气顶部的A1EE的变化主要依赖于单散射的Albedo,而表面的相同变化依赖于颗粒尺寸。对阴霾时期气溶胶的详细调查可以帮助我们进一步了解局部气候变化和阴霾诱导机制。

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  • 作者单位

    State Key Laboratory of Information Engineering in Surveying Mapping and Remote Sensing Wuhan University Wuhan China;

    Hubei Key Laboratory of Critical Zone Evolution School of Geography and Information Engineering China University of Geosciences Wuhan China;

    State Key Laboratory of Information Engineering in Surveying Mapping and Remote Sensing Wuhan University Wuhan China;

    State Key Laboratory of Information Engineering in Surveying Mapping and Remote Sensing Wuhan University Wuhan China;

    Department of Physics Stevens Institute of Technology Hoboken NJ USA;

    Hubei Provincial Meteorological Bureau Wuhan China;

    State Key Laboratory of Information Engineering in Surveying Mapping and Remote Sensing Wuhan University Wuhan China;

    State Key Laboratory of Information Engineering in Surveying Mapping and Remote Sensing Wuhan University Wuhan China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

    Long‐Term Investigation; Aerosol Optical; Radiative Characteristics;

    机译:长期调查;气溶胶光学;辐射特性;

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