考虑到 HydroGNSS,结合全球导航卫星系统反射测量法和机器学习绘制 5 千米全球土壤湿度图

IF 5.7 Q1 ENVIRONMENTAL SCIENCES
Emanuele Santi , Davide Comite , Laura Dente , Leila Guerriero , Nazzareno Pierdicca , Maria Paola Clarizia , Nicolas Floury
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引用次数: 0

摘要

鉴于计划于 2024 年发射的欧空局 HydroGNSS 飞行任务,本研究探讨了利用 GNSS-R 观测数据绘制全球尺度和相对较高分辨率(约 0.05°,相当于约 5 千米)的土壤和植被参数图的可能性。05° (大约相当于 5 公里)的 SM 地图的可能性,具体方法是实施和比较两种基于机器学习技术的检索算法,即人工神经网络(ANN)和随机森林回归器(RF)。在等待水文全球导航卫星系统调试和运行期间,美国国家航空航天局的旋风全球导航卫星系统(CyGNSS)陆地观测数据被考虑用于这一范围。利用这两种机器学习技术的多功能性,对包括 CyGNSS 观测数据和辅助信息在内的多种输入数据组合进行了开发,并对 GNSS-R 和辅助数据的作用进行了评估。鉴于缺乏 0.05°分辨率的全球 SM 数据,采用了以下新策略来建立训练集:首先,将 EASE-Grid 36 公里上的 SMAP SM 作为目标,在较低分辨率下进行训练。然后,将训练好的算法应用于 0.05°的 CyGNSS 数据,以获得该分辨率的全球 SM 地图。最后,0.05°的SM与ISMN进行了验证,以尽可能保持训练和验证的独立性。两种检索技术显示出相似的精确度和计算成本,全球计算的估计 SM 与目标 SM 之间的相关系数 R ≃0.9,RMSE ≃0.05(m3/m3)。此外,0.05° 的 SM 地图显示了一些更精细的细节和小尺度模式,而 36 公里处的 SMAP 原始 SM 数据没有显示这些细节和模式。无论采用哪种多层面技术,这项研究都证实,与微波卫星辐射计提供的 SM 产品相比,GNSS-R 在提高分辨率对 SM 进行全球监测方面具有巨大潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Global soil moisture mapping at 5 km by combining GNSS reflectometry and machine learning in view of HydroGNSS
The potential of GNSS reflectometry (GNSS-R) for the monitoring of soil and vegetation parameters as soil moisture (SM) and forest aboveground biomass (AGB) has been largely investigated in recent years.
In view of the ESA's HydroGNSS mission, planned to be launched in 2024, this study has explored the possibility to map SM at global scale and relatively high resolution of about 0.05° (corresponding approximately to 5 Km) using GNSS-R observations, by implementing and comparing two retrieval algorithms based on machine learning techniques, namely Artificial Neural Networks (ANN) and Random Forest Regressors (RF). Waiting for HydroGNSS commissioning and operation, the NASA's Cyclone GNSS (CyGNSS) land observations have been considered for this scope. Taking advantage of the versatility of both machine learning techniques, several combinations of input data, including CyGNSS observables and auxiliary information, have been exploited and the role of GNSS-R and auxiliary data has been assessed. Given the lack of global SM data at 0.05° resolution, the following novel strategy has been implemented to establish the training set: as first, training has been carried out at lower resolution by considering as target the SMAP SM on EASE-Grid 36 km. Then the trained algorithms have been applied to CyGNSS data at 0.05° to obtain global SM maps at this resolution. Finally, the SM at 0.05° has been validated against ISMN, to keep training and validation as much independent as possible. The two retrieval techniques exhibited similar accuracies and computational cost, with correlation coefficient R ≃ 0.9 between estimated and target SM computed globally, and RMSE ≃ 0.05 (m3/m3). Moreover, the SM maps at 0.05° revealed some finer details and small-scale patterns that are not shown by the original SMAP SM data at 36 km. Regardless of the ML technique applied, this study confirmed the promising potential of GNSS-R for the global monitoring of SM at improved resolution with respect to SM products available from microwave satellite radiometers.
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