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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Comparison of ground-based and remotely-sensed surface soil moisture estimates over complex terrain during SMEX04
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Comparison of ground-based and remotely-sensed surface soil moisture estimates over complex terrain during SMEX04

机译:SMEX04期间复杂地形上的地面和遥感地表土壤湿度估算值的比较

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Comparisons to ground-based surface soil moisture estimates are necessary to evaluate the capability of remote sensors to determine Soil moisture and its spatiotemporal variability. Soil moisture can be especially variable in regions of complex terrain which exhibit large variations in vegetation, soil properties and hydrologic conditions. The objective of this study is to evaluate the spatiotemporal variability of soil moisture in a mountainous basin in northwestern Mexico. Soil moisture estimates from ground sampling over a topographic transect and high resolution retrievals from the Polarimetric Scanning Radiometer are compared during a two week period in August 2004 as part of the Soil Moisture Experiment 2004. Results indicate that the soil moisture estimates exhibit similar variability with mean water content. Statistical analysis, however, reveals clear differences in soil moisture in the basin, in particular for wet periods and high elevations. Despite these differences, the temporal persistence of soil moisture from the estimates agrees well and indicates locations that capture the basin-averaged conditions. Furthermore, the spatiotemporal soil moisture characteristics from the two products are linked to terrain attributes. As a result, a hypsometric technique is shown to improve comparisons between basin-averaged values derived from ground data and remote sensing, as compared to arithmetic averaging. To our knowledge, this study is the first attempt to evaluate PSR/CX retrievals with respect to ground observations over a region of high topographic and vegetation variability using statistical, time-stability and terrain analysis techniques. (C) 2007 Elsevier Inc. All rights reserved.
机译:必须与地面地面土壤湿度估算值进行比较,以评估遥感器确定土壤湿度及其时空变化的能力。在植被,土壤特性和水文条件表现出较大差异的复杂地形区域中,土壤水分尤其容易变化。这项研究的目的是评估墨西哥西北部山区盆地土壤水分的时空变化。作为2004年土壤水分实验的一部分,在2004年8月的两周期间,比较了地形样地的地面采样和极化扫描辐射计的高分辨率取回的土壤湿度估算值。结果表明,土壤湿度估算值的平均值具有相似的变化性含水量。然而,统计分析表明,流域内土壤水分的明显差异,特别是在潮湿时期和高海拔地区。尽管存在这些差异,但估算中的土壤水分在时间上的持久性非常吻合,并指出了捕获盆地平均条件的位置。此外,两种产品的时空土壤水分特征与地形属性有关。结果,与算术平均相比,显示了一种测压技术来改善从地面数据和遥感获得的盆地平均值之间的比较。就我们所知,这项研究是首次尝试使用统计,时间稳定性和地形分析技术,针对高地形和植被多变性地区的地面观测评估PSR / CX检索。 (C)2007 Elsevier Inc.保留所有权利。

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