Abstract

AbstractDownscaling is widely used in studies of local and/or regional climate as it yields a greater spatial resolution than general circulation models (GCMs) can provide. It utilizes GCM output or reanalysis data, which is transformed using mathematical relationships or used to force the lateral boundaries of a regional climate model. However, there is no set selection technique to determine which GCM realization(s) to employ. Here, a comprehensive yet easily applicable model selection technique for studies requiring GCM data as a constraint was developed. The technique evaluates, with respect to a reanalysis product and/or observational data, the ability of GCM realizations to reconstruct the mean state of the climate and the space‐time climatic anomalies for the atmospheric state variables at three distinct pressure levels. It was applied to the region of East Africa, where GISS‐E2‐H r6i1p3 was found to perform the strongest. The top ranked realizations were found to better capture processes when evaluated for the example of the Indian Ocean Dipole. Furthermore, the surface air temperature and precipitation from three 10‐year regional climate model simulations, one forced by the Modern‐Era Retrospective Analysis for Research and Applications version 2 reanalysis, one forced by the top ranked GCM, and one by the lowest ranked one, were compared to gridded observations. Results show that using a top ranked GCM for the boundary conditions leads to a better dynamical downscaling simulation than a low‐ranked GCM, suggesting the potential of the proposed technique for future downscaling techniques.

Highlights

  • General circulation models (GCMs), comprising atmosphere, land, and ocean components, are used to simulate large-scale climatic processes over various time periods

  • Other processes influence East African climate but, for brevity purposes, we focused on the how well the realizations represent the Indian Ocean Dipole (IOD) using the method outlined in Thielke and Mölg (2019)

  • We presented a model selection procedure to determine the suitability of general circulation models (GCMs) realizations for downscaling studies

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Summary

Introduction

General circulation models (GCMs), comprising atmosphere, land, and ocean components, are used to simulate large-scale climatic processes over various time periods Due to their coarse resolution, they cannot yield comprehensive simulations of climate at regional and local scales. Downscaling provides a great way to address this problem, since it leads to greater spatial resolution than GCMs can provide It can be divided into two distinct groups: statistical and dynamical. Dynamical downscaling involves forcing the lateral boundaries of a regional (atmospheric) climate model (RCM) with reanalysis data or GCM output This technique allows for local-scale processes (e.g., glacier mass balance, river/lake basin water levels) to be physically modeled from large-scale climate dynamics without circumventing any of the main scales (Giorgi, 2019; Giorgi & Bates, 1989)

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