Deep Learning Integrating Scale Conversion and Pedo‐Transfer Function to Avoid Potential Errors in Cross‐Scale Transfer

Author:

Li Peijun123ORCID,Zha Yuanyuan1ORCID,Zhang Yonggen4ORCID,Michael Tso Chak‐Hau56ORCID,Attinger Sabine78ORCID,Samaniego Luis78ORCID,Peng Jian23

Affiliation:

1. State Key Laboratory of Water Resources Engineering and Management Wuhan University Wuhan China

2. Department of Remote Sensing Helmholtz Centre for Environmental Research—UFZ Leipzig Germany

3. Remote Sensing Centre for Earth System Research Leipzig University Leipzig Germany

4. Institute of Surface‐Earth System Science School of Earth System Science Tianjin University Tianjin China

5. UK Centre for Ecology and Hydrology Lancaster UK

6. Lancaster Environment Centre Lancaster University Lancaster UK

7. Department of Computational Hydrosystems Helmholtz Centre for Environmental Research ‐ UFZ Leipzig Germany

8. Institute of Earth and Environmental Science‐Geoecology University of Potsdam Potsdam Germany

Abstract

AbstractPedo‐transfer functions (PTFs) relate soil/landscape static properties to a wide range of model inputs (e.g., soil hydraulic parameters) that are essential to soil hydrological modeling. Combining PTFs and hydrological models is a powerful strategy allowing the use of soil/landscape static properties for the generalization of large‐scale modeling. However, since the spatial scales of soil hydraulic parameters required for model inputs and soil/landscape static properties are often not identical, cross‐scale transfer is required, which can be a significant source of errors. Here, we investigate uncertainties in cross‐scale transfer and develop an approach that avoids them. The proposed method uses the convolutional neural network (CNN) as a cross‐scale transfer approach to directly map soil/landscape static properties to soil hydraulic parameters across different spatial scales. The proposed CNN approach is applied under two different estimation strategies to invert the hydraulic parameters of a soil‐water balance model and subsequently the quality of the parameters is assessed. Both synthetical and real‐world results around the conterminous United States indicate that in general the employed end‐to‐end strategy is superior to the two‐step strategy. The CNN‐based integrated model successfully reduces potential errors in cross‐scale transfer and can be applied to other areas lacking information on hydraulic parameters or observations. The proposed method can be extended to improve parameter estimation in earth system models and enhance our understanding of key hydrological processes.

Funder

National Natural Science Foundation of China

China Scholarship Council

Publisher

American Geophysical Union (AGU)

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1. Comment on “Are soils overrated in hydrology?” by Gao et al. (2023);Hydrology and Earth System Sciences;2024-09-06

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