Reconciling high resolution climate datasets using KrigR
Richard Davy, Erik Kusch

TL;DR
This paper demonstrates how the KrigR R-package can be used to statistically downscale ERA5 reanalysis data to high resolution, accurately capturing spatial heterogeneity and explaining differences among existing datasets.
Contribution
The study introduces a novel application of kriging via KrigR for high-resolution climate data downscaling, accounting for uncertainty and reconciling various datasets.
Findings
Kriging accurately recovers spatial heterogeneity with strong covariate relationships.
Uncertainty preservation allows confidence assessment in high-resolution data.
KrigR explains differences among CHELSA, TerraClimate, and WorldClim2 datasets.
Abstract
There is an increasing need for high spatial and temporal resolution climate data for the wide community of researchers interested in climate change and its consequences. Currently, there is a large mismatch between the spatial resolutions of global climate model and reanalysis datasets (at best around 0.25o and 0.1o respectively) and the resolutions needed by many end-users of these datasets, which are typically on the scale of 30 arcseconds (~900m). This need for improved spatial resolution in climate datasets has motivated several groups to statistically downscale various combinations of observational or reanalysis datasets. However, the variety of downscaling methods and inputs used makes it difficult to reconcile the resultant differences between these high-resolution datasets. Here we make use of the KrigR R-package to statistically downscale the world-leading ERA5(-Land)…
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