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Article title
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Abstract
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Keywords
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Introduction
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Background
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The Last Glacial Maximum as a benchmark period
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Proxy records
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Methods
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Workflow
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Temperature change (present-LGM) reconstruction based on paleoclimate datasets
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Temperature change (present-LGM) reconstruction based on global grid cooling
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Temperature change reconstruction vs proxy records
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Reconstruction of treeline elevations at the LGM
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Treeline definition
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LGM treeline reconstruction
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Results
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Spatial resolution of paleoclimate datasets
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LGM cooling estimates
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Comparison of reconstructed LGM treeline elevations
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Discussion
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Conclusions
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Acknowledgements
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Competing interest
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Author contributions
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Data availability statement
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References
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Supplementary material
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