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Global-scale streamflow simulation framework used in the paper of "Abrupt surface water decline during 2023–2024 record warming"

Domaine:

environment and energyclimate

Type de record:

software
Créateur:
ZhaLi,
Éditeur:
Zenodo
Hôte:avatar

Summary:

This repository contains the data and source code for a global-scale streamflow simulation framework utilizing an ensemble of machine learning models. The methodology addresses the challenge of hydrological variability by implementing a climate-zone-specific training approach. Results from the Step 3 script can be extrapolated globally to simulate monthly streamflow across all HydroSHEDS basins in the subsequent step.

Key technical features:

  • Specialized ensembles: The framework employs five machine learning architectures: Random Forest, Gradient Boosting, SVM, Neural Networks, and Gaussian Process Regression.
  • Climate segmentation: Basins are categorized using an Aridity Index (AI) threshold of 0.65.
  • Asymmetric weighting: To mitigate common overestimation issues in arid hydrology, dry-region models are trained with a 2x penalty for overestimation errors.
  • Bayesian Model Averaging (BMA): Individual model outputs are integrated using climate-zone-specific BMA weights to produce a robust final simulation.

Dataset contents:

  • Input data: Compiled monthly training features, observed monthly streamflow for 150 basins, optimized hyperparameters, and geospatial shapefiles.
  • Output data: Fully trained model objects, calibrated annual time series, and performance evaluation visualizations.
  • Source code: A comprehensive MATLAB script for data imputation, model training, and metric calculation (NSE, KGE, PBIAS) (see     
    step3_ML_DL_fulltraining_inputs_outputs_rep2.m)
    .

Temporal Coverage: 1991 – 2024.

Visit

doi.org

Languages

Ndasa

Tags

Machine learningBayesian Model AveragingStreamflowGlobal

Licenses

info:eu-repo/semantics/embargoedAccessCreative Commons Attribution 4.0 Internationalhttps://creativecommons.org/licenses/by/4.0/legalcode

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