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Benchmarking of topsoil moisture estimation methods based on a field study

Published online by Cambridge University Press:  20 January 2025

Sabina Thaler*
Affiliation:
Institute of Meteorology and Climatology, BOKU University, Vienna, Austria Global Change Research Institute Academy of Sciences of the Czech Republic, Brno, Czech Republic
Josef Eitzinger
Affiliation:
Institute of Meteorology and Climatology, BOKU University, Vienna, Austria
Milan Fischer
Affiliation:
Global Change Research Institute Academy of Sciences of the Czech Republic, Brno, Czech Republic
Gerhard Kubu
Affiliation:
Institute of Meteorology and Climatology, BOKU University, Vienna, Austria
David Marin
Affiliation:
Institute of Meteorology and Climatology, BOKU University, Vienna, Austria
Matěj Orság
Affiliation:
Global Change Research Institute Academy of Sciences of the Czech Republic, Brno, Czech Republic
Miroslav Trnka
Affiliation:
Global Change Research Institute Academy of Sciences of the Czech Republic, Brno, Czech Republic Institute of Agriculture Systems and Bioclimatology, Mendel University in Brno, Brno, Czech Republic
Filippo Vecchiotti
Affiliation:
Department of Gravitational Natural Hazards, GeoSphere Austria, Vienna, Austria
Mariette Vreugdenhil
Affiliation:
Department of Geodesy and Geoinformation, TU Wien, Vienna, Austria
Wolfgang Wagner
Affiliation:
Department of Geodesy and Geoinformation, TU Wien, Vienna, Austria
*
Corresponding author: Sabina Thaler; Email: sabina.thaler@boku.ac.at

Abstract

Extreme weather events caused by climate change, such as drought and heavy rainfall, will further increase in Central Europe in the near future. Resilient crop production requires in-depth knowledge of soil moisture (SM), its spatial and temporal variability and the dynamics of agriculturally used land. In the current study, different SM estimation methods, including measurement and simulation-based methods, were evaluated over a 17-ha experimental arable crop field with respect to their abilities to capture the spatial and temporal SM dynamics of within-field areas and their related uncertainty and spatial representativeness. The high-spatial resolution in-situ topsoil moisture measurements (50 m grid) were compared with the estimated SM from satellite-based remote sensing (S1ASCAT) and the simulated SM from three different crop water balance models (Agricultural Risk Information System [ARIS], AquaCrop and DSSAT). The evaluation revealed that the spatial variability in the experimental field obtained from the reference could not be captured by the alternative methods investigated because of the limitations of the grid size-related soil map information. Nevertheless, the analysis revealed a very good temporal correlation of SM dynamics with the field area average across all approaches, with AquaCrop and ARIS at a soil depth of 0–10 cm and S1ASCAT soil–water index 05 achieving a R2 and a Kling–Gupta efficiency >0.80. These results indicate the added value of complementary methods for estimating SM to reduce spatial and temporal uncertainties in the estimated topsoil water content.

Type
Crops and Soils Research Paper
Copyright
Copyright © The Author(s), 2025. Published by Cambridge University Press

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