TL;DR
This paper introduces a robust method to evaluate how climate proxies influence data assimilation-based paleoclimate reconstructions, revealing significant alterations in climate model states due to proxy assimilation and their increasing impact with more proxies.
Contribution
The paper presents a new functional data depth-based test to compare distributions of spatiotemporal climate fields, assessing proxy influence in data assimilation reconstructions.
Findings
Analysis states differ significantly from background states after proxy assimilation.
The difference between analysis and background increases with more proxies.
Proxies have a substantial impact even in regions far from collection sites.
Abstract
Climate field reconstructions (CFR) attempt to estimate spatiotemporal fields of climate variables in the past using climate proxies such as tree rings, ice cores, and corals. Data Assimilation (DA) methods are a recent and promising new means of deriving CFRs that optimally fuse climate proxies with climate model output. Despite the growing application of DA-based CFRs, little is understood about how much the assimilated proxies change the statistical properties of the climate model data. To address this question, we propose a robust and computationally efficient method, based on functional data depth, to evaluate differences in the distributions of two spatiotemporal processes. We apply our test to study global and regional proxy influence in DA-based CFRs by comparing the background and analysis states, which are treated as two samples of spatiotemporal fields. We find that the…
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