2011
DOI: 10.5194/gmdd-4-3295-2011
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Influence of parallel computational uncertainty on simulations of the Coupled General Climate Model

Abstract: This paper investigates the impact of the parallel computational uncertainty on climate simulations using the Community Climate System Model Version 3 (CCSM3). A series of sensitivity experiments have been conducted and the analyses are focused on the Global and Nino3.4 sea surface temperatures. It is shown that the amplitude of the deviation induced by the parallel computational uncertainty is the same order as that of the climate system change. However, the ensemble mean method can reduce the influenc… Show more

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Cited by 2 publications
(4 citation statements)
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“…Additionally, Figure 4d-9d indicate that model intercomparison analyses conducted on climatological (30 years) or decadal (10 years) timescales may be substantially influenced by the diversity of HPC platforms used to perform the simulations. This result is in contrast with what previously found by Song et al (2012), who stated that for (30-year) climatological means machine dependence uncertainty is negligible.…”
Section: The Physical Implicationscontrasting
confidence: 99%
See 2 more Smart Citations
“…Additionally, Figure 4d-9d indicate that model intercomparison analyses conducted on climatological (30 years) or decadal (10 years) timescales may be substantially influenced by the diversity of HPC platforms used to perform the simulations. This result is in contrast with what previously found by Song et al (2012), who stated that for (30-year) climatological means machine dependence uncertainty is negligible.…”
Section: The Physical Implicationscontrasting
confidence: 99%
“…The question to answer is whether the spread between the same set of ensemble members run on the ARCHER and MO platforms is any different. Song et al (2012) addressed the same question (using the Community Climate System Model Version 3) showing that a minimum of 15 ensemble members are needed to make machine dependence uncertainty negligible.…”
Section: The Physical Implicationsmentioning
confidence: 99%
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“…According to CMIP6 rules, for each numerical experiment, the ensembles are distinguished as “rKiLpMfN” by different numbers K, L, M, and N, which indicate different initial conditions, initialization methods, perturbed physics parameterizations and forcing, respectively, for the model configuration. The three realizations of historical run only differ in terms of initial conditions and are named r1i1p1f1, r2i1p1f1, and r3i1p1f1, respectively, and they have almost no effects on the climatological distribution and ENSO results (Song, Qiao, Lei, Wang, 2012). Therefore, in this paper, the time series analysis of historical simulation is applied to the ensemble mean and three realizations, while the first realization (r1i1p1f1) is analyzed for the evaluation of the climatological distribution and ENSO.…”
Section: Model Configurationmentioning
confidence: 99%