Joint probabilistic estimates of temperature and precipitation from tree ring-based reconstructions of the last millennium

Abstract. An understanding of Earth's past climate can help put current and future changes into historical context. Widely used tree ring-based drought atlases generally target the Palmer Drought Severity Index or other metrics of soil moisture and/or drought risk. These indices reflect contemporaneous meteorological conditions, and it is possible to extract information about temperature and precipitation given the existing reconstructions. Here, we present a fully Bayesian inverse method that infers a joint posterior for monthly mean temperature and precipitation given tree ring-based PDSI reconstructions from the North American Drought Atlas. The method is skillful at reconstructing early twentieth century conditions when compared to instrumental measurements from the CRU TS dataset. Moreover, the reconstructions can capture the complex temporal and multivariate covariance structure between monthly regional temperatures and precipitation. By reconstructing regional temperature and precipitation for the last millennium, we identify the driest and wettest years and decades in each region. Our results highlight the unique nature of the 1930s Dust Bowl drought in central Kansas and the late twentieth century pluvial in the North American southwest.

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Publication Details

Journal
Advances in statistical climatology, meteorology and oceanography
Published
2026-02-16
DOI
https://doi.org/10.5194/ascmo-12-43-2026
Primary Topic
Tree-ring climate responses
Type
article
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article

Joint probabilistic estimates of temperature and precipitation from tree ring-based reconstructions of the last millennium

Edward R. Cook, Ensheng Weng, Rina Singh, Kate Marvel et al.
Advances in statistical climatology, meteorology and oceanography
Tree-ring climate responses
article

Joint probabilistic estimates of temperature and precipitation from tree ring-based reconstructions of the last millennium

Edward R. Cook, Ensheng Weng, Rina Singh, Kate Marvel, Benjamin Cook
article en

Abstract

Abstract. An understanding of Earth's past climate can help put current and future changes into historical context. Widely used tree ring-based drought atlases generally target the Palmer Drought Severity Index or other metrics of soil moisture and/or drought risk. These indices reflect contemporaneous meteorological conditions, and it is possible to extract information about temperature and precipitation given the existing reconstructions. Here, we present a fully Bayesian inverse method that infers a joint posterior for monthly mean temperature and precipitation given tree ring-based PDSI reconstructions from the North American Drought Atlas. The method is skillful at reconstructing early twentieth century conditions when compared to instrumental measurements from the CRU TS dataset. Moreover, the reconstructions can capture the complex temporal and multivariate covariance structure between monthly regional temperatures and precipitation. By reconstructing regional temperature and precipitation for the last millennium, we identify the driest and wettest years and decades in each region. Our results highlight the unique nature of the 1930s Dust Bowl drought in central Kansas and the late twentieth century pluvial in the North American southwest.

Advances in statistical climatology, meteorology and oceanographyVol. 12(1)
Goddard Institute for Space Studies (US), Lamont-Doherty Earth Observatory (US), New York University (US), Columbia University (US)
Climate action
Openalex Percentile: Top 65%
Tree-ring climate responses
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