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TRUVACE RECORD VERSION record: TRV-2026-1217 version: 1 kind: certified reason: Certified into the record timestamp: 2026-09-30T06:55:40.063380Z status: published lens: trace sector: policy headline: Comparative hydro-climatic forecasting of reservoir storage and cross-scale bathymetric evaluation in Mingde and Shihmen reservoirs dek: Accurate reservoir storage forecasting is critical for water security and risk management, yet most data-driven approaches emphasize short-term predictive skill without accounting for long-term changes in storage capacity caused by sedimentation. This study addresses this gap by examining whether monthly, hydro-climatic machine learning forecasts of effective water storage capacity can be meaningfully evaluated against observed, multi-year capacity changes derived from bathymetric surveys. Forecasting performanc… gain_title: Monthly hydro-climatic machine learning models reproduced observed storage variability at two Taiwan reservoirs with high Nash-Sutcliffe efficiency when static capacity curves were assumed. problem_title: Same hydro-climatic models failed to capture multi-year effective capacity loss from sedimentation when benchmarked against bathymetric surveys, producing relative errors up to 292% and systematic bias in droughts. trace_subject: monthly hydro-climatic machine learning forecasting of effective water storage capacity at Mingde and Shihmen reservoirs in Taiwan gain_reading: Monthly hydro-climatic machine learning models reproduced observed storage variability at two Taiwan reservoirs with high Nash-Sutcliffe efficiency when static capacity curves were assumed. gain_evidence: linear model provides stable and accurate forecasts (Nash-Sutcliffe efficiency of 0.968) problem_reading: Same hydro-climatic models failed to capture multi-year effective capacity loss from sedimentation when benchmarked against bathymetric surveys, producing relative errors up to 292% and systematic bias in droughts. problem_evidence: failure to capture multi-year capacity loss caused by sedimentation, with relative errors reaching up to 292% quick_read: By September 2026, a peer-reviewed study tested monthly hydro-climatic machine learning forecasts of effective storage at Mingde and Shihmen reservoirs in Taiwan, comparing linear regularized regression and a nonlinear tree-based model against observed storage and multi-year bathymetric capacity changes. The work matters because high short-term skill (NSE 0.968 at Mingde, 0.952 at Shihmen) coexisted with large long-term errors when sedimentation was ignored, leaving uncertainty about how to integrate sediment transport, land-use, and operational releases that were unavailable at monthly resolution. limitation: Framework relies only on hydro-climatic forcing and static capacity curves, so it cannot account for sedimentation-driven capacity change and is biased during extremes. tag: Dual reading key_points: Study evaluated linear regularized regression and nonlinear tree-based models forced by precipitation, temperature, humidity, and evaporation at Mingde and Shihmen reservoirs in Taiwan. | Interpretability analysis found forecasts dominated by antecedent storage, causing systematic bias during extreme drought conditions. | Authors deliberately excluded monthly sediment transport, land-use, and operational release records due to temporal unavailability or static nature. rundown: Researchers forced both models with precipitation, temperature, humidity, and evaporation and evaluated them with conventional metrics plus independent bathymetric benchmarking and interpretability analysis at rainfall-driven Mingde and highly regulated Shihmen. Benchmarking against multi-year bathymetric surveys showed accurate reproduction of storage variability under static capacity assumptions but inability to track sedimentation-induced capacity decline, indicating need to incorporate sediment processes for long-term management. sources: - peer_reviewed | Environmental Science and Pollution Research | https://doi.org/10.1007/s11356-026-38246-1 | 2026-09-28 prev: 0000000000000000000000000000000000000000000000000000000000000000
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