Abstract

Abstract. This paper proposes a criterion for deciding whether climate model simulations are consistent with observations. Importantly, the criterion accounts for correlations in both space and time. The basic idea is to fit each multivariate time series to a vector autoregressive (VAR) model and then test the hypothesis that the parameters of the two models are equal. In the special case of a first-order VAR model, the model is a linear inverse model (LIM) and the test constitutes a difference-in-LIM test. This test is applied to decide whether climate models generate realistic internal variability of annual mean North Atlantic sea surface temperature. Given the disputed origin of multidecadal variability in the North Atlantic (e.g., some studies argue it is forced by anthropogenic aerosols, while others argue it arises naturally from internal variability), the time series are filtered in two different ways appropriate to the two driving mechanisms. In either case, only a few climate models out of three dozen are found to generate internal variability consistent with observations. In fact, it is shown that climate models differ not only from observations, but also from each other, unless they come from the same modeling center. In addition to these discrepancies in internal variability, other studies show that models exhibit significant discrepancies with observations in terms of the response to external forcing. Taken together, these discrepancies imply that, at the present time, climate models do not provide a satisfactory explanation of observed variability in the North Atlantic.

Highlights

  • A basic question in climate modeling is whether a given model realistically simulates observations

  • Shown is the deviance between ERSST 1854–1936 and ERSST 1937–2018. The latter deviance falls below the 5 % threshold and indicates no significant difference in internal variability between two halves of ERSST, regardless of polynomial fit

  • One CMIP5 model is consistent with ERSST when a second-order polynomial is removed, and only two CMIP5 models are consistent with ERSST when a ninth-order polynomial is removed

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Summary

Introduction

A basic question in climate modeling is whether a given model realistically simulates observations. In the special case of a single random variable and independent samples, this question can be addressed by applying standard tests of equality of distributions, such as the t test, F test, or Kolmogorov–Smirnov test. In many climate studies, multiple variables are of concern, and the associated time series are serially correlated. For such time series, these standard tests are not meaningful. The above question arises often in the context of North Atlantic sea surface temperature (NASST) variability. The North Atlantic is an area of enhanced decadal predictability and a prime candidate for skillful predictions on multiyear timescales (Kushnir, 1994; Griffies and Bryan, 1997; Marshall et al, 2001; Latif et al, 2004, 2006; Keenlyside et al, 2008).

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