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Methodological study demonstrates improved variance estimation in climate attribution, highlighting more reliable uncertainty quantification for regional warming trends.
Climate change detection and attribution plays a central role in establishing the influence of human activities on global warming. The widely used optimal fingerprinting framework can be formulated as a linear errors-in-variables regression in which the covariance of internal climate variability is estimated from climate model simulations. Existing regularized optimal fingerprinting approaches often underestimate the variance of the scaling factors, leading to confidence intervals that are too narrow and fail to achieve nominal coverage. In this paper, we first propose consistent variance estimators for the regression coefficients within the general class of linear shrinkage weight matrices, thereby addressing the undercoverage problem in conventional methods. Building on this result, we further derive a linearly optimal weight matrix that directly minimizes the asymptotic variances of the estimated scaling factors. Numerical studies confirm improved empirical coverage and shorter interval lengths. When applied to annual mean near-surface air temperature (1951–2020), the proposed method produces narrower and more reliable intervals and provides new insights in detection and attribution across different regional scales.
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Li et al. (2026) studied this question.
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