Earth System Dynamics Discussions | 2019

Evaluating climate emulation: fundamental impulse testing of simple climate models

 
 
 
 
 
 

Abstract


Abstract. Simple climate models\xa0(SCMs) are numerical representations of the Earth s gas cycles and climate system. SCMs are easy to use and computationally inexpensive, making them an ideal tool in both scientific and decision-making contexts (e.g., complex climate model emulation, parameter estimation experiments, climate metric calculations, and probabilistic analyses). Despite their prolific use, the fundamental responses of SCMs are often not directly characterized. In this study, we use fundamental impulse tests of three chemical species ( CO2 , CH4 , and\xa0black carbon – BC) to understand the fundamental gas cycle and climate system responses of several comprehensive (Hector\xa0v2.0, MAGICC\xa05.3, MAGICC\xa06.0) and idealized (FAIR\xa0v1.0, AR5-IR) SCMs. We find that while idealized SCMs are widely used, they fail to capture the magnitude and timescales of global mean climate responses under emissions perturbations, which can produce biased temperature results. Comprehensive SCMs, which have physically based nonlinear forcing and carbon cycle representations, show improved responses compared to idealized SCMs. Even the comprehensive SCMs, however, fail to capture the response timescales to BC\xa0emission perturbations seen recently in two general circulation models. Some comprehensive SCMs also generally respond faster than more complex models to a 4×CO2 concentration perturbation, although this was not evident for lower perturbation levels. These results suggest where improvements should be made to SCMs. Further, we demonstrate here a set of fundamental tests that we recommend as a standard evaluation suite for any SCM. Fundamental impulse tests allow users to understand differences in model responses and the impact of model selection on results.

Volume 10
Pages 729-739
DOI 10.5194/esd-10-729-2019
Language English
Journal Earth System Dynamics Discussions

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