分析p波段SAR信号的二面体散射分量以估计主干介电常数——一个概念研究

IF 5.7 Q1 ENVIRONMENTAL SCIENCES
Anke Fluhrer , Hamed Alemohammad , Thomas Jagdhuber
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引用次数: 0

摘要

提出了一种基于混合分解技术和扩展(x-)菲涅耳模型的树干介电常数反演方法。在2013年至2015年期间,利用NASA机载微波观测站(AirMOSS)的p波段SAR观测数据在美国各地的各个测量站测试了所提出的检索方法。为了测试x-菲涅耳模型用于此类分析的可行性及其对所需输入参数的灵敏度,详细的灵敏度研究表明,在p波段频率下,需要考虑散射损失、相位差以及由于表面粗糙度引起的潜在退极化效应。分解的二面体散射分量随植被覆盖度的增加而增加,从一个站点(控制站)的荒地到均匀森林站点(目标站)。总的来说,二面体散射量与估计的主干介电常数之间没有明显的相关性,这是由于所采用方法的结构所导致的。采用该方法估算的干流介电常数在2.4 ~ 59.7[-]之间,其中荒地和森林密度较低的站点的干流介电常数较低。在这些台站,二面体散射不是SAR总信号的主要散射机制,这违背了所提出方法的物理特性。在二面体散射占优势的站点,树干介电常数与AMSR2相对含水量(RWC)、MODIS蒸散发(ET)、实测相对湿度(RH)和气温(Tair)之间存在合理的相关关系(r值在±0.1 ~±0.64之间)。这些参数用于分析所提出方法的可行性,因为所调查的站点和年份没有现场干流湿度测量数据。因此,具有足够高的二面体散射部分的p波段SAR观测可用于估计主干介电常数,并扩展遥感在气候研究中的潜在应用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analyzing the dihedral scattering component of P-band SAR signals for trunk permittivity estimation – a concept study
A new retrieval method, based on a hybrid decomposition technique and the extended (x-) Fresnel model, is proposed for estimating trunk permittivity from polarimetric P-band SAR observations. P-band SAR observations of NASA's Airborne Microwave Observatory of Subcanopy and Subsurface (AirMOSS) mission campaign are employed to test the proposed retrieval method at individual measuring stations across the U.S. between 2013 and 2015. In order to test the feasibility of the x-Fresnel model for such analyses and its sensitivity to required input parameters, a detailed sensitivity study revealed that at P-band frequencies there is a need to account for scattering losses, phase differences, as well as potential depolarization effects due to surface roughness. The decomposed dihedral scattering component increases with increasing vegetation cover from barren land at one station (control station) to homogeneously forested stations (target stations). Overall, no clear correlation between the amount of dihedral scattering and estimated trunk permittivity could be found, which is expected due to the architecture of the employed method. With the proposed approach, the estimated trunk permittivity varies between 2.4 and 59.7 [-], where the barren land and less dense forested stations show lower trunk permittivity. At these stations, the dihedral scattering is not the dominant scattering mechanism within the total SAR signal, which violates the physics of the proposed approach. At stations with dominant dihedral scattering, reasonable correlations (with r ranging from ±0.1 to ±0.64) between estimated trunk permittivity and AMSR2 relative water content (RWC), MODIS evapotranspiration (ET), in-situ measured relative humidity (RH), and air temperature (Tair) could be found. These parameters are used for analyzing the feasibility of the proposed approach as no in-situ trunk moisture measurements are available for the investigated stations and years. Hence, P-band SAR observations that exhibit sufficiently high dihedral scattering portions can be used for estimating trunk permittivity and extend the potential applications of remote sensing for climate research.
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