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首页> 外文期刊>Journal of geophysical research. Earth Surface: JGR >A review of snow and ice albedo and the development of a newphysically based broadband albedo parameterization
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A review of snow and ice albedo and the development of a newphysically based broadband albedo parameterization

机译:冰雪反照率及其基于宽带的反照率参数化研究进展

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摘要

We present a computationally simple, theoretically based parameterization for thebroadband albedo of snow and ice that can accurately reproduce the theoretical broadbandalbedo under a wide range of snow, ice, and atmospheric conditions. Depending on itsapplication, this parameterization requires between one and five input parameters. Theseparameters are specific surface area of snow/ice, concentration of light-absorbing carbon,solar zenith angle, cloud optical thickness, and snow depth. The parameterization isderived by fitting equations to albedo estimates generated with a 16-stream plane-parallel,discrete ordinates radiative transfer model of snow and ice that is coupled to a similarmodel of the atmosphere. Output from this model is also used to establish the physicaldeterminants of the spectral albedo of snow and ice and evaluate the characteristics ofspectral irradiance over snow-covered surfaces. Broadband albedo estimates determinedfrom the radiative transfer model are compared with results from a selection of previouslyproposed parameterizations. Compared to these parameterizations, the newly proposedparameterization produces accurate results for a much wider range of snow, ice, andatmospheric conditions.
机译:我们为雪和冰的宽带反照率提出了一种计算简单,基于理论的参数设置,可以在广泛的雪,冰和大气条件下准确地再现理论的宽带反照率。根据其应用,此参数化需要一到五个输入参数。这些参数是雪/冰的比表面积,吸光碳的浓度,太阳天顶角,云的光学厚度和雪深。通过对方程进行拟合来拟合参数化,以将16流平行且离散的雪和冰的辐射传递模型与相似的大气模型耦合生成的反照率估计值。该模型的输出还用于建立冰雪光谱反照率的物理决定因素,并评估积雪表面上的光谱辐照度特征。从辐射传输模型确定的宽带反照率估计值与先前建议的参数化结果进行比较。与这些参数化相比,新提出的参数化可在更广泛的雪,冰和大气条件下产生准确的结果。

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