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SMRT: an active–passive microwave radiative transfer model for snow with multiple microstructure and scattering formulations (v1.0)

机译:SMRT:一种具有多种微观结构和散射公式的雪的主动-被动微波辐射传递模型(v1.0)

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The Snow Microwave Radiative Transfer (SMRT) thermal emission and backscatter model was developed to determine uncertainties in forward modeling through intercomparison of different model ingredients. The model differs from established models by the high degree of flexibility in switching between different electromagnetic theories, representations of snow microstructure, and other modules involved in various calculation steps. SMRT v1.0 includes the dense media radiative transfer theory (DMRT), the improved Born approximation (IBA), and independent Rayleigh scatterers to compute the intrinsic electromagnetic properties of a snow layer. In the case of IBA, five different formulations of the autocorrelation function to describe the snow microstructure characteristics are available, including the sticky hard sphere model, for which close equivalence between the IBA and DMRT theories has been shown here. Validation is demonstrated against established theories and models. SMRT was used to identify that several former studies conducting simulations with in situ measured snow properties are now comparable and moreover appear to be quantitatively nearly equivalent. This study also proves that a third parameter is needed in addition to density and specific surface area to characterize the microstructure. The paper provides a comprehensive description of the mathematical basis of SMRT and its numerical implementation in Python. Modularity supports model extensions foreseen in future versions comprising other media (e.g., sea ice, frozen lakes), different scattering theories, rough surface models, or new microstructure models.
机译:开发了Snow Microwave Radiative Transfer(SMRT)热发射和反向散射模型,以通过对不同模型成分进行比较来确定前向建模中的不确定性。该模型与已建立的模型的不同之处在于,在不同电磁理论,雪微结构表示以及各种计算步骤中涉及的其他模块之间进行切换时具有高度的灵活性。 SMRT v1.0包括密集介质辐射传输理论(DMRT),改进的伯恩近似(IBA)和独立的瑞利散射体,用于计算雪层的固有电磁特性。对于IBA,可以使用五种不同的自相关函数公式来描述雪的微结构特征,包括粘性硬球模型,此处显示了IBA和DMRT理论之间的等效性。根据既定的理论和模型证明了验证。使用SMRT可以发现,一些以前的就地测量积雪性质进行模拟的研究现在具有可比性,而且从数量上看几乎是等效的。这项研究还证明,除了密度和比表面积以外,还需要第三个参数来表征微结构。本文全面介绍了SMRT的数学基础及其在Python中的数值实现。模块化支持在未来版本中预见的模型扩展,包括其他介质(例如,海冰,冰冻的湖泊),不同的散射理论,粗糙的表面模型或新的微结构模型。

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