首页> 外文期刊>Geoscience and Remote Sensing Letters, IEEE >Radar Retrieval of Surface and Deep Soil Moisture and Effect of Moisture Profile on Inversion Accuracy
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Radar Retrieval of Surface and Deep Soil Moisture and Effect of Moisture Profile on Inversion Accuracy

机译:地表和深层土壤水分的雷达反演及水分剖面对反演精度的影响

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We study the retrieval of surface and deep moisture of bare soil from noisy radar observations using simulated annealing. Due to moisture variations with depth, we model bare soil with a stratified dielectric profile with a rough surface on top. Small perturbation method (SPM) is used as the forward model. We use the full moisture profile for radar data synthesis and study the retrieval accuracy by varying the number of layers that represent the soil profile during inversion. The effect of measurement frequency on the accuracy of deep moisture retrieval is investigated. This work is intended for assessing the effect of subsurface profile on soil moisture retrieval from radar observations of NASA's Soil Moisture Active and Passive (SMAP) mission and future lower frequency airborne or spaceborne systems that may follow SMAP.
机译:我们使用模拟退火技术从嘈杂的雷达观测中研究了裸土表面和深层水分的反演。由于水分随深度的变化,我们对具有分层介电轮廓且顶部粗糙表面的裸土进行建模。小扰动法(SPM)被用作正向模型。我们将完整的湿度剖面用于雷达数据合成,并通过改变反演过程中代表土壤剖面的层数来研究检索精度。研究了测量频率对深层水分回收精度的影响。这项工作旨在通过NASA的土壤水分主动和被动(SMAP)任务以及可能遵循SMAP的未来低频机载或星载系统的雷达观测评估地下剖面对土壤水分获取的影响。

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