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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Multi-model radiometric slope correction of SAR images of complex terrain using a two-stage semi-empirical approach
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Multi-model radiometric slope correction of SAR images of complex terrain using a two-stage semi-empirical approach

机译:使用两阶段半经验方法的复杂地形SAR图像多模型辐射坡度校正

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摘要

Practical approaches for the implementation of terrain type dependent radiometric slope correction for SAR data are introduced. Radiometric slope effects are modelled as the products of two models. The first is a simple physical model based on the assumption of a uniform opaque layer of isotropic scatterers, which is independent of terrain type, frequency and polarization. It accounts for the slope-induced variation in the number of scatterers per resolution cell. The second is a semi-empirical model, which accounts for the variation in scattering mechanisms, dependent on terrain type, frequency and polarization. PALSAR FBD (L-band, HH- and HV-polarization) data are used at two test sites in Brazil and Fiji. Results for the Brazilian area, which has slopes up to 25 degrees, show that remaining slope effects for the multi-model case are much smaller than 0.1 dB, for all land cover types. This is much better than the best single-model approach where remaining slope effects can be very small for forests but be as large as 1.77 dB for woodland in HH-polarization. Results for the Fiji area, which has different vegetation types, are very similar. The potential large improvement, using this multi-model approach, in the accuracy of biomass estimation for transparent or open canopies is discussed. It is also shown that biomass change on slopes can be systematically under- or overestimated because of associated change in scattering mechanism. (C) 2014 Elsevier Inc. All rights reserved.
机译:介绍了针对SAR数据实施依赖于地形类型的辐射坡度校正的实用方法。辐射坡度效应被建模为两个模型的乘积。第一个是简单的物理模型,其基于各向同性散射体的不透明均匀层的假设,该层与地形类型,频率和极化无关。它解释了每个分辨率像元中由散射引起的斜率变化。第二个是半经验模型,该模型说明了散射机制的变化,具体取决于地形类型,频率和极化。在巴西和斐济的两个测试点使用了PALSAR FBD(L波段,HH和HV极化)数据。巴西地区的坡度最高为25度,结果表明,对于所有土地覆盖类型,多模型情况下的剩余坡度效应都远远小于0.1 dB。这比最好的单模型方法要好得多,后者在森林中,在HH极化时,剩余的坡度效应可能很小,而林地的剩余坡度效应可能高达1.77 dB。具有不同植被类型的斐济地区的结果非常相似。讨论了使用这种多模型方法在透明或开放冠层生物量估计准确性方面的潜在重大改进。还表明,由于散射机制的相关变化,可以系统地低估或高估斜坡上的生物量变化。 (C)2014 Elsevier Inc.保留所有权利。

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