Abstract

Obtaining large-scale, long-term, and spatial continuous soil moisture (SM) data is crucial for climate change, hydrology, and water resource management, etc. ESA CCI SM is such a large-scale and long-term SM (longer than 40 years until now). However, there exist data gaps, especially for the area of China, due to the limitations in remote sensing of SM such as complex topography, human-induced radio frequency interference (RFI), and vegetation disturbances, etc. The data gaps make the CCI SM data cannot achieve spatial continuity, which entails the study of gap-filling methods. In order to develop suitable methods to fill the gaps of CCI SM in the whole area of China, we compared typical Machine Learning (ML) methods, including Random Forest method (RF), Feedforward Neural Network method (FNN), and Generalized Linear Model (GLM) with a geostatistical method, i.e., Ordinary Kriging (OK) in this study. More than 30 years of passive–active combined CCI SM from 1982 to 2018 and other biophysical variables such as Normalized Difference Vegetation Index (NDVI), precipitation, air temperature, Digital Elevation Model (DEM), soil type, and in situ SM from International Soil Moisture Network (ISMN) were utilized in this study. Results indicated that: (1) the data gap of CCI SM is frequent in China, which is found not only in cold seasons and areas but also in warm seasons and areas. The ratio of gap pixel numbers to the whole pixel numbers can be greater than 80%, and its average is around 40%. (2) ML methods can fill the gaps of CCI SM all up. Among the ML methods, RF had the best performance in fitting the relationship between CCI SM and biophysical variables. (3) Over simulated gap areas, RF had a comparable performance with OK, and they outperformed the FNN and GLM methods greatly. (4) Over in situ SM networks, RF achieved better performance than the OK method. (5) We also explored various strategies for gap-filling CCI SM. Results demonstrated that the strategy of constructing a monthly model with one RF for simulating monthly average SM and another RF for simulating monthly SM disturbance achieved the best performance. Such strategy combining with the ML method such as the RF is suggested in this study for filling the gaps of CCI SM in China.

Highlights

  • Soil moisture (SM) is a measurement of water amount in an unsaturated soil zone.It is usually expressed as the ratio of water volume to the soil volume with a unit of cm3 /cm3

  • Such strategy combining with the Machine Learning (ML) method such as the Random Forest method (RF) is suggested in this study for filling the gaps of Climate Change Initiative (CCI) SM in China

  • We focus on filling data gaps of ESA CCI SM over the whole area of China

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Summary

Introduction

Soil moisture (SM) is a measurement of water amount in an unsaturated soil zone. It is usually expressed as the ratio of water volume to the soil volume (volumetric SM) with a unit of cm3 /cm. The record length should be greater than 30 years To fulfill this requirement, ESA developed a long-term SM product named ESA CCI SM through merging multiple active and passive microwave sensors. The data gaps associated with different satellite revisit times [2028] and the physical limitations in retrieving SM by microwave observations, such as complex topography, human-induced radio frequency interference (RFI), vegetation, or snow and ice, cannot be mitigated by increasing the number of sensors or improving the blending techniques [17]. The data gaps make the SM dataset discontinuous in space and time, which limits its application in supporting climate research [1], driving the hydrological model [2], and monitoring drought [6,7,8], etc This entails the development of gap-filling technology for ESA CCI SM [20]. The following sections introduced the details of the study methods and materials

Study Area
Gap-Filling Methods
Gap-filling Methods
Evaluation Methods
ESA CCI SM
Ancillary Materials
Evaluating the Gap-Filling Methods over the Whole Area of China
Methods over over Simulated
Spatial
Evaluating the at In Situ Stations
Three Strategies for Gap-filling based on RF
Comparisons of estimated
Conclusions
Full Text
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