Abstract
Multi-source soil moisture (SM) products provide a vigorous tool for the estimation of soil moisture on a large scale, but it is crucial to carry out the evaluation of those products before further application. In the present work, an evaluation framework on multi-source SM datasets over central and eastern agricultural areas of China was firstly proposed, based on a dense in situ SM monitoring network of 838 stations from 11 July 2012 to 31 December 2017. Each station adopted the most accurate gravimetric method for measuring the actual soil moisture. The effects of land use types and wet–dry conditions on the performances of multi-source SM products were further analyzed. Most satellite/reanalysis SM products could capture the spatial–temporal changes in soil moisture, especially for ERA5 products that matched the closest to the station-measured SM; by contrast, those satellite products showed poor spatial–temporal performances. Such phenomenon was also quantitatively demonstrated by the four statistical metrics correlation coefficient (CC), p-value, bias and root mean squared error (RMSE) between the satellite/reanalysis SM products and the ground-observed SM series. Further, most satellite/reanalysis SM products had poor performances in Forestland and Grassland areas, with a lower CC and a larger positive bias and RMSE. Such overestimation on soil moisture is possibly influenced by the inestimable parameter vegetation geometry and the vegetation water content in the radiative transfer models. The arid areas showed the worst CC between the station-observed SM data and different satellite/reanalysis SM products; meanwhile, the humid and semi-arid areas presented larger SM estimation errors than the other areas, especially for the satellite products. The fairly dry surface soil (arid area) and open water surface contamination (humid area) are suggested to hinder the reading of microwave-based retrieval systems. Additionally, the reanalysis SM products outperformed the satellite SM products in the evaluated areas, with better spatial–temporal performances, seasonality reflection and higher accuracy on SM estimation (higher CC, and lower bias and RMSE). This is because the reanalysis datasets assimilated various sources of datasets, especially the ground-observed data, with high quality. The evaluated results could provide guidance for fusing different satellite/reanalysis products, as a new feasible alternative to monitoring SM information in the future.
Highlights
Remote sensing techniques have shown huge advantages, which provide a vigorous tool for estimating soil moisture at high resolution both spatially and temporally and update data with short latency
The feasibility study of remote sensing technology for monitoring soil moisture is a hot issue in current research
Taylor diagrams were separately applied in four wet–dry areas, semihumid, humid, semi-arid and arid areas, which mainly considered the influences of spatial heterogeneity
Summary
Soil moisture (SM) is a key bridge in the interactions between the atmosphere, biosphere and hydrosphere, which influences the hydrologic cycle processes by controlling the partition of rainfall into surface runoff, infiltration and groundwater recharge, and the Remote Sens. Soil moisture information can be acquired through in situ observation instruments, or by remote sensing techniques. The in situ soil moisture instruments represent point-based monitoring, which can hardly obtain soil moisture information at regional to global scales, in some areas with uneven underlying surfaces of high spatial heterogeneity. Remote sensing techniques have shown huge advantages, which provide a vigorous tool for estimating soil moisture at high resolution both spatially and temporally and update data with short latency. The feasibility study of remote sensing technology for monitoring soil moisture is a hot issue in current research
Published Version (Free)
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have