https://essopenarchive.org/doi/full/10.22541/essoar.177316659.94398101/v1

*Authors: *Yue Wang, Daniele Visioni, Ben Kravitz, Douglas G MacMartin,
Dhruv Balwada

*10 March 2026*

*Abstract*
Machine learning (ML) models have shown considerable promise for the
statistical downscaling of climate projections; yet, their performance can
degrade under non-stationarity, when future climate statistics differ from
the historical data used for training. We systematically investigate this
problem by downscaling global temperature and precipitation fields from
coarser to higher resolutions across multiple emission pathways and solar
radiation modification (SRM) scenarios in the Max Planck Institute Earth
System Model. A U-Net trained directly on historical data exhibits
substantial degradation under future forcings, with the root-mean-square
error (RMSE) of the global-mean temperature time series increasing from
0.43$^\circ$C to 1.32$^\circ$C as scenario warming increases. To avoid
this, we propose a simple data preprocessing strategy that combines
residual learning with pixel-wise linear detrending and normalization to
mitigate distribution shift without architectural modifications. The
resulting stationary model reduces this RMSE to below 0.27$^\circ$C across
all scenarios, outperforms quantile delta mapping (QDM) in spatial and
temporal metrics, and runs 5–6 times faster. Downscaling SRM scenarios
presents distinct challenges compared to standard emission pathways,
leading to worse performance for some commonly used downscaling methods.
Finally, we present the first ML-based global downscaling of a
Geoengineering Model Intercomparison Project (GeoMIP) SRM simulation,
generating extra-high-resolution (0.25$^\circ$) monthly temperature
projections for the G6sulfur scenario to support better regional impact
assessments of SRM, as well as to provide a benchmark for further localized
downscaling efforts.

*Source: ESS OPEN ARCHIVE *

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