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首页> 外文期刊>Selected Topics in Applied Earth Observations and Remote Sensing, IEEE Journal of >A New Fusion Algorithm for Simultaneously Improving Spatio-Temporal Continuity and Quality of Remotely Sensed Soil Moisture Over the Tibetan Plateau
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A New Fusion Algorithm for Simultaneously Improving Spatio-Temporal Continuity and Quality of Remotely Sensed Soil Moisture Over the Tibetan Plateau

机译:一种新的融合算法,以同时提高藏高高原遥感土壤水分的时空连续性和质量

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摘要

Spatio-temporally continuous and high-quality soil moisture (SM) is very important for assessing changes in the water cycle and climate, especially over the Tibetan plateau (TP). Data fusion is an important method to improve the quality of SM product. However, limited observation overlaps between different satellite SM products, caused by inherent gaps, make it difficult to fuse them to create a continuous and high-quality product. In this study, an SM spatio-temporal continuity and quality simultaneously improving algorithm is proposed. The first step of the approach is obtaining spatio-temporally continuous reference data, including land surface temperature (LST), normalized difference vegetation index (NDVI), Albedo, and digital elevation model (DEM). The second step is training the general regression neural network (GRNN) model with all available essential climate variables (ECV) and Fengyun (FY) SM. The last step is predicting the spatio-temporally continuous and high-quality SM using the trained GRNN derived by the spatio-temporal continuity reference data. An implementation of the algorithm on the TP showed that, compared with the original ECV and FY SM, both the continuity and quality of the fused SM product were largely improved in terms of coverage (72.5%), correlation ( R = 0.809), root mean square error (0.081 cm 3 cm −3 ) and bias (0.050 cm 3 cm −3 ). The algorithm showed a good performance in obtaining spatio-temporal variation fusion weights over the TP. This spatio-temporally continuous and high-quality SM of the TP will help advance our understanding of global and regional changes in water cycle and climate.
机译:时空连续和高质量的土壤水分(SM)对于评估水循环和气候的变化非常重要,特别是在西藏高原(TP)上。数据融合是提高SM产品质量的重要方法。然而,由固有的间隙引起的不同卫星SM产品之间的有限观察重叠,使得熔化它们难以熔化,以创造连续和高质量的产品。在该研究中,提出了SM时空连续性和质量同时提高算法。该方法的第一步是获得时空连续参考数据,包括陆地温度(LST),归一化差异植被指数(NDVI),Albedo和数字高度模型(DEM)。第二步是通过所有可用的基本气候变量(ECV)和Fengyun(FY)SM培训一般回归神经网络(GRNN)模型。最后一步是使用由时空连续性参考数据衍生的训练的GRNN预测时空连续和高质量的SM。 TP上的算法的实现表明,与原始ECV和FY SM相比,融合SM产品的连续性和质量都在覆盖范围(72.5%),相关性(<斜体​​XMLNS:MML = “http://www.w3.org/1998/math/mathml”xmlns:xlink =“http://www.w3.org/1999/xlink”> r = 0.809),均均匀误差(0.081 cm 3 cm -3 )和偏见(0.050 cm 3 cm - 3 )。该算法在获得TP上获得时空变化融合权重的良好性能。 TP的这种时空连续和高质量的SM将有助于推进我们对水循环和气候的全球和区域变化的理解。

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