Spatiotemporal functional permutation tests for comparing observed climate behavior to climate model projections

Abstract. Comparisons of observed and modeled climate behavior often focus on central tendencies, which overlook other important distributional characteristics related to quantiles and variability. We propose two permutation procedures, standard and stratified, for assessing the accuracy of climate models. Both procedures eliminate the need to model cross-correlations in the data, encouraging their application in a variety of contexts. By making only slightly stronger assumptions, the stratified procedure dramatically strengthens the ability to detect a difference in the distribution of observed and climate model data. The proposed procedures allow researchers to identify potential model deficiencies over space and time for a variety of distributional characteristics, providing a more comprehensive assessment of climate model accuracy, which will hopefully lead to further model refinements. The proposed statistical methodology is applied to temperature data generated by the state-of-the-art North American Coordinated Regional Climate Downscaling Experiment (NA-CORDEX).

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Publication Details

Journal
Advances in statistical climatology, meteorology and oceanography
Published
2024-10-02
DOI
https://doi.org/10.5194/ascmo-10-123-2024
Citations
2
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
0.57

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article

Spatiotemporal functional permutation tests for comparing observed climate behavior to climate model projections

Piotr Kokoszka, Joshua P. French, Seth McGinnis
2 citations
Advances in statistical climatology, meteorology and oceanography
Climate variability and models
0.57
article

Spatiotemporal functional permutation tests for comparing observed climate behavior to climate model projections

Piotr Kokoszka, Joshua P. French, Seth McGinnis
article en
2 citations

Abstract

Abstract. Comparisons of observed and modeled climate behavior often focus on central tendencies, which overlook other important distributional characteristics related to quantiles and variability. We propose two permutation procedures, standard and stratified, for assessing the accuracy of climate models. Both procedures eliminate the need to model cross-correlations in the data, encouraging their application in a variety of contexts. By making only slightly stronger assumptions, the stratified procedure dramatically strengthens the ability to detect a difference in the distribution of observed and climate model data. The proposed procedures allow researchers to identify potential model deficiencies over space and time for a variety of distributional characteristics, providing a more comprehensive assessment of climate model accuracy, which will hopefully lead to further model refinements. The proposed statistical methodology is applied to temperature data generated by the state-of-the-art North American Coordinated Regional Climate Downscaling Experiment (NA-CORDEX).

Advances in statistical climatology, meteorology and oceanographyVol. 10(2)
NSF National Center for Atmospheric Research (US), University of Colorado Denver (US), Colorado State University (US)
Directorate for Mathematical and Physical Sciences
Climate action
Openalex Percentile: Top 33%
Climate variability and models
0.57
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Spatiotemporal functional permutation tests for comparing observed climate behavior to climate model projections — Piotr Kokoszka, Joshua P. French, et al. · Advances in statistical climatology, meteorology and oceanography (2024) | TGRS Research Map | TGRS