Comparing climate time series – Part 2: A multivariate test

Q1 Mathematics
T. DelSole, M. Tippett
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引用次数: 3

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.
比较气候时间序列。第2部分:多变量检验
摘要本文提出了一个判定气候模式模拟是否与观测相一致的准则。重要的是,该标准考虑了空间和时间上的相关性。其基本思想是将每个多变量时间序列拟合到一个向量自回归(VAR)模型中,然后检验两个模型参数相等的假设。在一阶VAR模型的特殊情况下,模型是线性逆模型(LIM),检验构成LIM中的差异检验。该检验用于确定气候模式是否产生真实的北大西洋海表年平均温度的内部变率。鉴于北大西洋多年代际变率的起源存在争议(例如,一些研究认为它是由人为气溶胶造成的,而另一些研究认为它是由内部变率自然产生的),时间序列以两种不同的方式进行过滤,以适应两种驱动机制。在任何一种情况下,在36个气候模式中,只有少数模式被发现产生与观测一致的内部变率。事实上,气候模式不仅与观测不同,而且彼此之间也不同,除非它们来自同一个模式中心。除了这些内部变率的差异之外,其他研究表明,模式在对外部强迫的响应方面与观测结果存在显著差异。综上所述,这些差异意味着,目前气候模式不能对观测到的北大西洋变率提供令人满意的解释。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Advances in Statistical Climatology, Meteorology and Oceanography
Advances in Statistical Climatology, Meteorology and Oceanography Earth and Planetary Sciences-Atmospheric Science
CiteScore
4.80
自引率
0.00%
发文量
9
审稿时长
26 weeks
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