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Evaluation of ground-based remotely sensed liquid water cloud properties using shortwave radiation measurements

机译:利用短波辐射测量评估地面遥感液态水云的特性

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摘要

Water cloud optical and microphysical properties are required for a better understanding of the impact of aerosols on the solar radiation feedback. The introduced retrieval technique provides droplet concentration, effective radius and optical thickness on a basis of ground-based remote sensing observations and a vertical cloud model. Mainly cloud radar, microwave radiometer and ceilometer observations are used in this approach. The model assumptions are related to a sub-adiabatic approach, in which cloud mixing processes are predefined to be homogeneous. A gamma droplet size distribution with a fixed shape parameter is considered to relate the observations with the retrieval products. The technique is applied on a water cloud case and the uncertainties in relation to the model assumptions and errors in the measurements are determined. The greatest uncertainty in the retrieval of droplet concentration is related to the fixed shape parameter, which requires in-situ data for validation processes to quantify the results. The optical parameters are less sensitive to the model assumptions and they are evaluated with a radiative closure experiment. They are used as input for radiative transfer calculations in order to compare the simulations with radiation measurements at the ground. There is a relatively good agreement between the simulated and measured radiation considering the horizontal cloud inhomogeneity, although a bias of around 5% still exists. Therefore the technique might be a suitable approach of retrieving quantitative cloud optical properties independently from radiation observations.
机译:需要水云的光学和微物理特性,以更好地了解气溶胶对太阳辐射反馈的影响。引入的检索技术在基于地面的遥感观测和垂直云模型的基础上提供了液滴浓度,有效半径和光学厚度。这种方法主要使用云雷达,微波辐射计和云高仪观测。模型假设与亚绝热方法有关,其中将云混合过程预定义为同质的。具有固定形状参数的伽玛液滴尺寸分布被认为将观测值与检索结果相关联。将该技术应用于水云情况,并确定与模型假设和测量误差有关的不确定性。液滴浓度检索中的最大不确定性与固定形状参数有关,该参数需要用于验证过程的现场数据来量化结果。光学参数对模型假设不太敏感,并通过辐射封闭实验对其进行了评估。它们用作辐射传输计算的输入,以便将模拟与地面辐射测量值进行比较。考虑到水平云的不均匀性,在模拟辐射和测量辐射之间有相对较好的一致性,尽管仍存在大约5%的偏差。因此,该技术可能是一种独立于辐射观测来检索定量云光学特性的合适方法。

著录项

  • 来源
    《Atmospheric research》 |2010年第3期|P.366-377|共12页
  • 作者单位

    International Research Center for Telecommunication and Radar, Delft University of Technology, Mekelweg 4,2628 CD Delft, The Netherlands;

    rnInternational Research Center for Telecommunication and Radar, Delft University of Technology, Mekelweg 4,2628 CD Delft, The Netherlands;

    Royal Netherlands Meteorological Institute, Wilhelminalaan 10, 3732 GK De Bilt, The Netherlands;

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

    water clouds; droplet concentration; optical thickness; radiation feedback;

    机译:水云液滴浓度光学厚度辐射反馈;
  • 入库时间 2022-08-18 03:36:06

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