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Simulation of microwave emission and backscattering of layered snowpacks by a radiative transfer model, and validation by surface-based experiments

机译:通过辐射传递模型模拟层状积雪的微波发射和反向散射,并通过基于地面的实验进行验证

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A thermal microwave emission model of layered snowpacks (MEMLS) has been previously developed for the frequency range, 5 to 100 GHz. It is based on six-flux radiative transfer to describe multiple volume scattering, absorption, and refractive effects. MEMLS is a physical model with a semi-empirical part in the description of the scattering coefficient, and later this element was completed by a fully physical scattering theory. Model validation included surface-based radiometer experiments and detailed in-situ data. In a further step to be presented in the present article the authors tested MEMLS by using Chandrasekhar's H-functions. They show how they can be applied to a refractive medium such as snow. As an effect of refraction a Lambert-like behavior is obtained. Since the formalism is bistatic, it also delivers the backscattering coefficient, yielding the link to radar data. Data from active and passive microwave experiments will be used to test the models.
机译:先前已经针对5至100 GHz的频率范围开发了分层积雪的热微波发射模型(MEMLS)。它基于六通量辐射传递来描述多重体积散射,吸收和折射效应。 MEMLS是描述散射系数的具有半经验部分的物理模型,后来这个元素由完全物理散射理论完成。模型验证包括基于地面的辐射计实验和详细的原位数据。在本文要介绍的另一个步骤中,作者使用Chandrasekhar的H函数测试了MEMLS。它们展示了如何将其应用于折射介质(例如雪)。作为折射的效果,获得了类似朗伯的行为。由于形式主义是双基地的,因此它还提供了反向散射系数,从而建立了与雷达数据的链接。来自主动和被动微波实验的数据将用于测试模型。

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