Abstract

Abstract. Land surface models are typically integrated into global climate projections, but as their spatial resolution increases the prospect of using them to aid in local policy decisions becomes more appealing. If these complex models are to be used to make local decisions, then a full quantification of uncertainty is necessary, but the computational cost of running just one full simulation at high resolution can hinder proper analysis. Statistical emulation is an increasingly common technique for developing fast approximate models in a way that maintains accuracy but also provides comprehensive uncertainty bounds for the approximation. In this work, we developed a statistical emulation framework for land surface models, enabling fast predictions at a high resolution. To do so, our emulation framework acknowledges, and makes use of, the multitude of contextual data that are often fed into land surface models (sometimes called forcing data, or driving data), such as air temperature or various soil properties. We use The Joint UK Land Environment Simulator (JULES) as a case study for this methodology, and perform initial sensitivity analysis and parameter tuning to showcase its capabilities. The JULES is perhaps one of the most complex land surface models and so our success here suggests incredible gains can be made for all types of land surface model.

Highlights

  • Land surface models (LSMs) represent the terrestrial biosphere within weather and climate models, focusing on hydrometeorology and biogeophysical coupling with the atmosphere

  • It is an essential part of the process to check the accuracy of an emulator, just as it is with the LSM itself

  • We have outlined a framework for emulating land surface models (LSM) using sparse Gaussian processes (GP)

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Summary

Introduction

Land surface models (LSMs) represent the terrestrial biosphere within weather and climate models, focusing on hydrometeorology and biogeophysical coupling with the atmosphere. The latter includes nutrient flows between vegetation and soils, and the turbulent exchange of CO2, heat, moisture, and momentum between the land surface and the atmosphere. The LSMs can be used to further scientific understanding of land surface processes and to inform policy decisions. For both applications, increased confidence in simulated results and knowledge of model uncertainty is needed, which typically involves running the model many times with varied forcings and parameters (Booth et al, 2012; Murphy et al, 2004). The computational cost of running these models limits the number of runs that can be obtained, constraining the resulting analysis

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