Spatial downscaling of precipitation using adaptable random forests

Xiaogang He, Nathaniel W. Chaney, Marc Schleiss, Justin Sheffield

Water Resources Research · 2016 · 269 citations · 69 references

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TL;DR

This paper proposes Prec‑DWARF, a machine‑learning approach that uses adaptable random forests to statistically downscale precipitation. Prec‑DWARF builds a nonlinear mapping between fine‑resolution precipitation and multi‑scale covariates via Random Forests, optionally employing two independent RFs to better capture extremes, and is evaluated on hourly NLDAS‑2 gauge‑radar data at 0.125° across 0.25°, 0.5°, and 1° resolutions. Evaluation shows Prec‑DWARF outperforms bilinear interpolation, accurately reproducing precipitation patterns, though single‑RF models underestimate extremes and fine‑scale structure, while double‑RF models improve extremes yet still under‑estimate variability; key predictors are neighboring coarse precipitation and distance to dry cells, underscoring the method’s potential.

Abstract

This paper introduces Prec-DWARF (Precipitation Downscaling With Adaptable Random Forests), a novel machine-learning based method for statistical downscaling of precipitation. Prec-DWARF sets up a nonlinear relationship between precipitation at fine resolution and covariates at coarse/fine resolution, based on the advanced binary tree method known as Random Forests (RF). In addition to a single RF, we also consider a more advanced implementation based on two independent RFs which yield better results for extreme precipitation. Hourly gauge-radar precipitation data at 0.125° from NLDAS-2 are used to conduct synthetic experiments with different spatial resolutions (0.25°, 0.5°, and 1°). Quantitative evaluation of these experiments demonstrates that Prec-DWARF consistently outperforms the baseline (i.e., bilinear interpolation in this case) and can reasonably reproduce the spatial and temporal patterns, occurrence and distribution of observed precipitation fields. However, Prec-DWARF with a single RF significantly underestimates precipitation extremes and often cannot correctly recover the fine-scale spatial structure, especially for the 1° experiments. Prec-DWARF with a double RF exhibits improvement in the simulation of extreme precipitation as well as its spatial and temporal structures, but variogram analyses show that the spatial and temporal variability of the downscaled fields are still strongly underestimated. Covariate importance analysis shows that the most important predictors for the downscaling are the coarse-scale precipitation values over adjacent grid cells as well as the distance to the closest dry grid cell (i.e., the dry drift). The encouraging results demonstrate the potential of Prec-DWARF and machine-learning based techniques in general for the statistical downscaling of precipitation.

References

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