Application potential and spatiotemporal uncertainty assessment of multi-layer soil moisture estimation in different climate zones using multi-source data

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Journal of Hydrology Pub Date : 2024-10-28 DOI:10.1016/j.jhydrol.2024.132229
Jiaxin Qian , Jie Yang , Weidong Sun , Lingli Zhao , Lei Shi , Hongtao Shi , Chaoya Dang , Qi Dou
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Abstract

Accurately estimating multi-layer soil moisture (SM) through remote sensing methods presents inherent challenges and limitations. Multi-layer SM provides valuable insights into the intricate interactions within the “soil-vegetation-atmosphere” system. This study explored the temporal dynamics of multi-layer SM in the Shandian River Basin, China, from 2019 to 2020. Through sensitivity analysis, we demonstrated the feasibility of using multi-source data for estimating multi-layer SM, including dual polarization radar data, optical vegetation descriptors, terrain factors, soil parameters, and meteorological indices. Initially, surface soil moisture (SSM) at depths of 3 cm and 5 cm was estimated using the modified change detection (MCD) model, which reduces the impact of vegetation. Incorporating constraints from soil parameters during the solving process improved the estimation accuracy of multi-layer SM. Subsequently, the water balance model, involving precipitation and evaporation, was applied to further correct the estimation results of SSM. Based on this, the infiltration process was considered to estimate deeper SM, including near-surface soil moisture (NSSM) at depths of 10 cm and 20 cm, and root zone soil moisture (RZSM) at depths of 40–50 cm. Under this framework, the estimation errors for multi-layer SM were satisfactory (RMSE = 0.041–0.045 cm3/cm3). Finally, we explored the upper limits of multi-layer SM estimation using multi-input and multi-output machine learning regression (MLR) algorithms. With the incorporation of multi-source data, advanced MLR algorithms achieved higher estimation accuracy (RMSE = 0.015–0.022 cm3/cm3) and showed potential for cross-temporal transfer (RMSE = 0.030–0.037 cm3/cm3). Moreover, spatiotemporal robustness revalidation of multi-layer SM was conducted across 17 observation networks distributed cross different climatic zones in China. The results shown that the MCD model achieved satisfactory results in estimating multi-layer SM (RMSE = 0.053–0.064 cm3/cm3), whereas the regression models displayed higher accuracy (RMSE = 0.039–0.051 cm3/cm3). Both the MCD and MLR models yielded similar conclusions, indicating that the estimation accuracy of NSSM and RZSM surpassed that of SSM, primarily due to the relatively lower variability of the former and their strong coupling with vegetation productivity. This study also specifically discussed the influence of factors such as radar incidence angles, soil texture types, and vegetation types on the estimation accuracy of multi-layer SM. This study introduced a novel concept and framework for regional multi-layer and profile SM estimation and real-time prediction through multi-source data, exhibiting high potential for practical applications.
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利用多源数据进行不同气候区多层土壤水分估算的应用潜力和时空不确定性评估
通过遥感方法精确估算多层土壤湿度(SM)存在固有的挑战和局限性。多层土壤水分为了解 "土壤-植被-大气 "系统内错综复杂的相互作用提供了宝贵的信息。本研究探讨了 2019 年至 2020 年中国山甸河流域多层土壤水分的时间动态。通过灵敏度分析,我们证明了使用多源数据估算多层土壤水分的可行性,包括双偏振雷达数据、光学植被描述符、地形因子、土壤参数和气象指数。最初,使用修正的变化探测(MCD)模型估算了 3 厘米和 5 厘米深度的表层土壤湿度(SSM),该模型减少了植被的影响。在求解过程中加入土壤参数的约束条件,提高了多层土壤水分的估算精度。随后,应用涉及降水和蒸发的水平衡模型进一步修正了 SSM 的估算结果。在此基础上,考虑渗透过程来估算深层土壤水分,包括 10 厘米和 20 厘米深度的近表层土壤水分(NSSM)以及 40-50 厘米深度的根区土壤水分(RZSM)。在此框架下,多层土壤水分的估算误差令人满意(RMSE = 0.041-0.045 cm3/cm3)。最后,我们利用多输入和多输出机器学习回归(MLR)算法探索了多层 SM 估算的上限。随着多源数据的加入,先进的 MLR 算法实现了更高的估计精度(RMSE = 0.015-0.022 cm3/cm3),并显示出跨时空转移的潜力(RMSE = 0.030-0.037 cm3/cm3)。此外,还对分布于中国不同气候带的 17 个观测网络进行了多层 SM 的时空鲁棒性再验证。结果表明,MCD 模型在估算多层 SM 方面取得了令人满意的结果(RMSE = 0.053-0.064 cm3/cm3),而回归模型则显示出更高的精度(RMSE = 0.039-0.051 cm3/cm3)。MCD 和 MLR 模型得出的结论相似,表明 NSSM 和 RZSM 的估算精度超过 SSM,主要原因是前者的变异性相对较低,且与植被生产力的耦合度较高。本研究还具体讨论了雷达入射角、土壤质地类型和植被类型等因素对多层土壤扫描估算精度的影响。本研究通过多源数据为区域多层和剖面 SM 估算和实时预测引入了一个新的概念和框架,具有很高的实际应用潜力。
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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