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Published on: October 11, 2018
Decomposition of the mean absolute error (MAE) into systematic and unsystematic components
Scott M Robeson1, Cort J Willmott2
1Department of Geography, Indiana University, Bloomington, Indiana, United States of America.
This study introduces a new three-part decomposition for the mean absolute error (MAE), offering a more interpretable way to assess quantitative model performance compared to traditional sums-of-squares methods.
Area of Science:
- Hydrology
- Quantitative Modeling
- Error Analysis
Background:
- Quantitative model performance is often evaluated using sums-of-squares error metrics like Mean Squared Error (MSE) and Root Mean Squared Error (RMSE).
- While MSE/RMSE are mathematically tractable for decomposition, Mean Absolute Error (MAE) offers superior interpretability for quantifying average error.
- Existing MSE decompositions provide insights into systematic and unsystematic error components.
Purpose of the Study:
- To develop and demonstrate a novel decomposition of MAE into three distinct error submeasures.
- To provide a more interpretable alternative to MSE-based error decompositions for quantitative models.
- To enhance the understanding of model-error distributions.
Main Methods:
- Developed a three-part decomposition for MAE, comprising bias error, proportionality error, and unsystematic error.
- Applied this decomposition to a long-term streamflow reconstruction dataset.
- Illustrated the properties and benefits of the new MAE decomposition.
Main Results:
- The proposed MAE decomposition effectively separates model error into bias, proportionality, and unsystematic components.
- This method offers clearer insights into the nature of model-error distributions than MSE-based decompositions.
- The decomposition was successfully illustrated using streamflow data from the Upper Colorado River.
Conclusions:
- The three-part MAE decomposition provides a more intuitive and informative assessment of quantitative model performance.
- This approach enhances the interpretability of model errors, aiding in model improvement.
- The method is broadly applicable to various quantitative modeling applications, particularly in hydrology.
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