Assimilation of Time-Averaged Pseudoproxies for Climate Reconstruction
Assimilation of Time-Averaged Pseudoproxies for Climate Reconstruction
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DOI:
10.1175/jcli-d-12-00693.1
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发表时间:
2014-01
影响因子:
4.9
通讯作者:
N. Steiger;G. Hakim;E. Steig;D. Battisti;G. Roe
中科院分区:
文献类型:
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作者:
N. Steiger;G. Hakim;E. Steig;D. Battisti;G. Roe
The efficacy of a novel ensemble data assimilation (DA) technique is examined in the climate field reconstruction (CFR) of surface temperature. A minimalistic, computationally inexpensive DA technique is employed that requires only a static ensemble of climatologically plausible states. Pseudoproxy experiments are performed with both general circulation model (GCM) and Twentieth Century Reanalysis (20CR) data byreconstructingsurfacetemperaturefieldsfromasparsenetworkofnoisypseudoproxies.TheDAapproach is compared to a conventional CFR approach based on principal component analysis (PCA) for experiments on global domains. DA outperforms PCA in reconstructing global-mean temperature in all experiments and is more consistent across experiments, with a range of time series correlations of 0.69‐0.94 compared to 0.19‐ 0.87 for the PCA method. DA improvements are even more evident in spatial reconstruction skill, especially in sparsely sampled pseudoproxy regions and for 20CR experiments. It is hypothesized that DA improves spatialreconstructionsbecauseitreliesoncoherent,spatiallylocaltemperaturepatterns,whichremainrobust even when glacial states are used to reconstruct nonglacial states and vice versa. These local relationships, as utilized by DA, appear to be more robust than the orthogonal patterns of variability utilized by PCA. Comparing results for GCM and 20CR data indicates that pseudoproxy experiments that rely solely on GCM data may give a false impression of reconstruction skill.