On the value of mobile cosmic-ray neutron measurements for spatio-temporal soil moisture simulations

High-resolution soil moisture measurements are indispensable for advancing hydrological modeling and improving environmental risk assessments at regional scales. However, it remains an open question to what level hydrological models are capable of representing spatio-temporal patterns of root-zone soil moisture. In this study, we present a novel integration of mobile Cosmic-Ray Neutron Sensor (CRNS) data collected via rail-based measurements into the mesoscale Hydrologic Model (mHM). Over ten months, daily CRNS observations had been acquired along a 9-km railway corridor and subsequently aggregated to a ~ 200 m, spatial resolution to align with the mHM resolution. Soil moisture related model parameters were optimized for distinct land cover types based on observed soil moisture dynamics, including dense forest, open forest, meadow, and railway shunting areas. Model simulations exhibited considerable improvements with Nash-Sutcliffe Efficiency (NSE) values increasing from −0.19 to 0.76 in the dense forest, and from 0.50 to 0.79 in the meadow with homogeneous land cover conditions. In contrast, areas characterized by mixed land use—such as half-open forests and railway yards exhibited lower performance, indicating areas of improvements in the model-data fusion scheme including higher resolution that may be necessary to fully capture local variability. Further, results of the spatio-temporal analysis demonstrated the model ability to reproduce observed spatial patterns of CRNS derived soil moisture with the spatial efficiency (SPAEF) score of 0.71 (1.0 being an ideal one). Finally, the transferability of the optimized parameters was evaluated by applying them to independent sites located 38–345 km away from the original measurement corridor. The reasonably good agreement between simulated and observed soil moisture at grassland sites further confirms the robustness and applicability of our model-data fusion approach, while substantial biases remain in forest sites. Overall, the integration of mobile CRNS measurements represents a new era for hydrological modeling by providing unprecedented spatial resolution and temporal coverage to facilitate more precise soil moisture estimations for effective water resource management, and forecasting of floods and droughts.

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Publication Details

Journal
Frontiers in Water
Published
2025-11-03
DOI
https://doi.org/10.3389/frwa.2025.1630051
Citations
1
Primary Topic
Soil Moisture and Remote Sensing
Type
article
Field-Weighted Citation Impact
0.80

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On the value of mobile cosmic-ray neutron measurements for spatio-temporal soil moisture simulations

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On the value of mobile cosmic-ray neutron measurements for spatio-temporal soil moisture simulations

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article en
1 citations

Abstract

High-resolution soil moisture measurements are indispensable for advancing hydrological modeling and improving environmental risk assessments at regional scales. However, it remains an open question to what level hydrological models are capable of representing spatio-temporal patterns of root-zone soil moisture. In this study, we present a novel integration of mobile Cosmic-Ray Neutron Sensor (CRNS) data collected via rail-based measurements into the mesoscale Hydrologic Model (mHM). Over ten months, daily CRNS observations had been acquired along a 9-km railway corridor and subsequently aggregated to a ~ 200 m, spatial resolution to align with the mHM resolution. Soil moisture related model parameters were optimized for distinct land cover types based on observed soil moisture dynamics, including dense forest, open forest, meadow, and railway shunting areas. Model simulations exhibited considerable improvements with Nash-Sutcliffe Efficiency (NSE) values increasing from −0.19 to 0.76 in the dense forest, and from 0.50 to 0.79 in the meadow with homogeneous land cover conditions. In contrast, areas characterized by mixed land use—such as half-open forests and railway yards exhibited lower performance, indicating areas of improvements in the model-data fusion scheme including higher resolution that may be necessary to fully capture local variability. Further, results of the spatio-temporal analysis demonstrated the model ability to reproduce observed spatial patterns of CRNS derived soil moisture with the spatial efficiency (SPAEF) score of 0.71 (1.0 being an ideal one). Finally, the transferability of the optimized parameters was evaluated by applying them to independent sites located 38–345 km away from the original measurement corridor. The reasonably good agreement between simulated and observed soil moisture at grassland sites further confirms the robustness and applicability of our model-data fusion approach, while substantial biases remain in forest sites. Overall, the integration of mobile CRNS measurements represents a new era for hydrological modeling by providing unprecedented spatial resolution and temporal coverage to facilitate more precise soil moisture estimations for effective water resource management, and forecasting of floods and droughts.

Frontiers in WaterVol. 7
Helmholtz Centre for Environmental Research (DE), University of Potsdam (DE), Czech University of Life Sciences Prague (CZ)
Deutscher Akademischer Austauschdienst, Deutsche Forschungsgemeinschaft
Openalex Percentile: Top 23%
Soil Moisture and Remote Sensing
0.80
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