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Climate of the last millennium: ensemble consistency of simulations and reconstructions

机译:上个千年的气候:模拟和重建的整体一致性

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Are simulations and reconstructions of past climate and its variabilityconsistent with each other? We assess the consistency of simulations andreconstructions for the climate of the last millennium under the paradigm ofa statistically indistinguishable ensemble. In this type of analysis, thenull hypothesis is that reconstructions and simulations are statisticallyindistinguishable and, therefore, are exchangeable with each other. Ensembleconsistency is assessed for Northern Hemisphere mean temperature, CentralEuropean mean temperature and for global temperature fields. Reconstructionsavailable for these regions serve as verification data for a set ofsimulations of the climate of the last millennium performed at the Max PlanckInstitute for Meteorology.Consistency is generally limited to some sub-domains and some sub-periods.Only the ensemble simulated and reconstructed annual Central European meantemperatures for the second half of the last millennium demonstratesunambiguous consistency. Furthermore, we cannot exclude consistency of anensemble of reconstructions of Northern Hemisphere temperature with thesimulation ensemble mean.If we treat simulations and reconstructions as equitable hypotheses aboutpast climate variability, the found general lack of their consistency weakensour confidence in inferences about past climate evolutions on the consideredspatial and temporal scales. That is, our available estimates of past climateevolutions are on an equal footing but, as shown here, inconsistent with eachother.
机译:过去气候及其变异性的模拟和重建是否相互一致?我们在统计上无法区分的合奏范式下,评估了上个千年的气候模拟和重建的一致性。在这种类型的分析中,综合假设是,重建和模拟在统计上是无法区分的,因此可以相互交换。对北半球平均温度,中欧平均温度和全球温度场进行整体一致性评估。这些区域可用的重建数据是马克斯·普朗克气象研究所进行的一系列最近千年气候模拟的验证数据。 一致性通常仅限于某些子域和某些子时段。整体模拟和重建了上个千年下半年的中欧年度平均温度,显示出前后一致。此外,我们不能排除北半球温度重构与模拟总体平均值的一致性。在过去的气候变化中所考虑的时空尺度。就是说,我们对过去气候演变的现有估计是平等的,但是,如此处所示,彼此之间不一致。

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