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Upscaling sparse ground-based soil moisture observations for the validation of coarse-resolution satellite soil moisture products

机译:稀疏基于地面的土壤水分观测,用于验证粗分辨率卫星土壤水分产品

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摘要

The contrast between the point-scale nature of current ground-based soil moisture instrumentation and the ground resolution (typically >10 2 km 2) of satellites used to retrieve soil moisture poses a significant challenge for the validation of data products from current and upcoming soil moisture satellite missions. Given typical levels of observed spatial variability in soil moisture fields, this mismatch confounds mission validation goals by introducing significant sampling uncertainty in footprint-scale soil moisture estimates obtained from sparse ground-based observations. During validation activities based on comparisons between ground observations and satellite retrievals, this sampling error can be misattributed to retrieval uncertainty and spuriously degrade the perceived accuracy of satellite soil moisture products. This review paper describes the magnitude of the soil moisture upscaling problem and measurement density requirements for ground-based soil moisture networks. Since many large-scale networks do not meet these requirements, it also summarizes a number of existing soil moisture upscaling strategies which may reduce the detrimental impact of spatial sampling errors on the reliability of satellite soil moisture validation using spatially sparse ground-based observations. © 2012 by the American Geophysical Union.
机译:当前基于地面的土壤水分测量仪器的点标度性质与用于获取土壤水分的卫星的地面分辨率(通常> 10 2 km 2)之间的对比对验证当前和即将来临的土壤中的数据产品提出了重大挑战湿度卫星任务。给定典型水平的土壤水分观测空间变异性,这种失配会因从稀疏的地面观测获得的足迹规模土壤水分估算中引入明显的采样不确定性而混淆了任务验证目标。在基于地面观测和卫星取回之间比较的验证活动中,这种采样误差可能会归因于取回的不确定性,并会虚假地降低卫星土壤水分产品的感知精度。这篇综述文章描述了土壤水分升级问题的严重程度以及地面土壤水分网络的测量密度要求。由于许多大型网络都不能满足这些要求,因此它还总结了许多现有的土壤水分放大策略,这些策略可以减少使用空间稀疏的地面观测数据对卫星土壤水分验证的可靠性造成的不利影响。 ©2012,美国地球物理联盟。

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