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Published on: December 9, 2012
Differences in extremes and uncertainties in future runoff simulations using SWAT and LSTM for SSP scenarios
Young Hoon Song1, Eun-Sung Chung1, Shamsuddin Shahid2
1Faculty of Civil Engineering, Seoul National University of Science and Technology, 232 Gongneung-ro, Nowon-gu, Seoul 01811, Republic of Korea.
This study compared Long Short-Term Memory networks (LSTM) and Soil Water Assessment Tool (SWAT) for hydrological modeling. LSTM showed better performance in simulating observed runoff, while SWAT projected increased future runoff.
Area of Science:
- Hydrology
- Climate Science
- Machine Learning
Background:
- Accurate hydrological modeling is crucial for water resource management.
- Climate change necessitates reliable projections of future runoff.
- Comparing deep learning (LSTM) and physically-based (SWAT) models offers insights into hydrological simulation capabilities.
Purpose of the Study:
- To compare the performance of LSTM and SWAT in simulating and projecting runoff.
- To evaluate model capabilities under different climate change scenarios (SSPs).
- To assess model uncertainties in historical and future runoff estimations.
Main Methods:
- Utilized 11 CMIP6 Global Climate Models (GCMs) with bias correction via quantile mapping.
- Employed LSTM and SWAT for runoff simulation and projection for SSPs 2-4.5 and 5-8.5.
- Quantified uncertainties using Bayesian Model Averaging (BMA) and reliability ensemble averaging (REA).
Main Results:
- Bias-corrected GCMs significantly improved climate variable replication.
- LSTM demonstrated superior performance over SWAT in reproducing observed runoff.
- SWAT projected a 17.7% increase, while LSTM projected a 13.6% decrease in future runoff.
Conclusions:
- LSTM exhibits greater potential for accurate runoff simulation compared to SWAT.
- Model uncertainties differ between historical and projected periods, and between models.
- Findings provide valuable perspectives on deep learning versus physically-based models in hydrological applications.
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