Root zone soil moisture mapping at very high spatial resolution using radar-derived surface soil moisture product

IF 5.9 1区 农林科学 Q1 AGRONOMY
Nadia Ouaadi , Abdelghani Chehbouni , Emna Ayari , Bouchra Ait Hssaine , Jamal ElFarkh , Michel Le Page , Salah Er-Raki , Aaron Boone
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引用次数: 0

Abstract

Root zone soil moisture (RZSM) is a key variable controlling the soil-vegetation-atmosphere exchanges. Its estimation is vital for monitoring hydrological, meteorological and agricultural processes. A number of large-scale products exist but with a coarse resolution (>1 km), which is not suitable for plot-scale studies. The aim of this work is to map RZSM, for the first time, at very high spatial resolution using a very high spatial resolution surface soil moisture (SSM) product and a recursive exponential filter. SSM is estimated from Sentinel-1 data using the water cloud model at a resolution of approximately 50 m. The approach was evaluated on a database consisting of 12 fields, including 7 winter wheat and 5 summer maize fields, irrigated using different techniques. The results show that the approach performs reasonably well using Sentinel-1 SSM product with correlation coefficient (R) between 0.3 and 0.82, root-mean-square error (RMSE) between 0.05 and 0.12 m3/m3 and a bias in the range −0.1–0.07 m3/m3, at 15–20 cm depth. This is equivalent to R = 0.6, RMSE = 0.12 m3/m3 and bias = 0.07 m3/m3 using the entire database, which is quite low compared to the use of in situ SSM measurements (R = 0.81, RMSE = 0.07 m3/m3 and bias = 0.03 m3/m3). This is related to inaccuracies in the SSM product, where fields with good SSM estimation also resulted in good RZSM estimation and conversely. In addition to SSM, the approach is also sensitive to its time constant T. Analysis of RZSM sensitivity to T shows that the optimum T value depends on soil texture, climate and measurement depth. In particular, low optimum T values (1 day) are obtained for loamy and sandy loam soils, while higher values (5–10 days) are optimal for soils with a high clay fraction, at 15–20 cm depth. These values increase with soil depth and are influenced by seasonal atmospheric demand. Combined to reasonable statistical metrics, the spatial variability depicted by the RZSM maps opens up prospects for high-resolution RZSM mapping from Sentinel-1 SSM data using a simple approach over annual crops. This is of prime relevance for agricultural applications requiring very high-resolution estimation at plot scale, such as crop yield, irrigation and fertilizer management, as well as for the assessment of inter-plot variability.
利用雷达导出的地表土壤水分产品进行高空间分辨率的根区土壤水分制图
根区土壤水分是控制土壤-植被-大气交换的关键变量。它的估算对于监测水文、气象和农业过程至关重要。存在一些大尺度产品,但分辨率较粗(>1 km),不适合进行图尺度研究。这项工作的目的是首次使用非常高空间分辨率的地表土壤湿度(SSM)产品和递归指数滤波器在非常高的空间分辨率下绘制RZSM。SSM是根据Sentinel-1数据使用分辨率约为50 m的水云模式估计的。该方法在一个数据库中进行了评价,该数据库包含12块农田,其中包括7块冬小麦田和5块夏玉米田,采用不同的灌溉技术。结果表明,在15-20 cm深度,Sentinel-1 SSM产品的相关系数(R)在0.3 ~ 0.82之间,均方根误差(RMSE)在0.05 ~ 0.12 m3/m3之间,偏差在−0.1 ~ 0.07 m3/m3之间,该方法具有较好的效果。这相当于使用整个数据库的R = 0.6,RMSE = 0.12 m3/m3和偏差= 0.07 m3/m3,与使用原位SSM测量相比,这是相当低的(R = 0.81, RMSE = 0.07 m3/m3和偏差= 0.03 m3/m3)。这与SSM产品中的不准确性有关,其中具有良好SSM估计的字段也会产生良好的RZSM估计,反之亦然。除SSM外,该方法对其时间常数T也很敏感。RZSM对T的敏感性分析表明,最佳T值取决于土壤质地、气候和测量深度。特别是,壤土和砂质壤土的最佳T值较低(1 天),而粘土含量高的土壤在15-20 cm深度处的最佳T值较高(5-10天)。这些值随土壤深度的增加而增加,并受季节大气需求的影响。结合合理的统计指标,RZSM地图所描述的空间变异性为利用Sentinel-1 SSM数据对一年生作物使用简单方法进行高分辨率RZSM制图开辟了前景。这对于需要在地块尺度上进行非常高分辨率估计的农业应用,例如作物产量、灌溉和肥料管理,以及评估地块间变异性具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Agricultural Water Management
Agricultural Water Management 农林科学-农艺学
CiteScore
12.10
自引率
14.90%
发文量
648
审稿时长
4.9 months
期刊介绍: Agricultural Water Management publishes papers of international significance relating to the science, economics, and policy of agricultural water management. In all cases, manuscripts must address implications and provide insight regarding agricultural water management.
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