500-year paleoclimate record inferred from Greenland Juniper wood contextualizes current climate warming
Status PubMed-not-MEDLINE Jazyk angličtina Země Anglie, Velká Británie Médium electronic
Typ dokumentu časopisecké články
Grantová podpora
UMO-2019/35/D/ST10/03137
Narodowe Centrum Nauki (National Science Centre)
PubMed
41298452
PubMed Central
PMC12749314
DOI
10.1038/s41467-025-66842-1
PII: 10.1038/s41467-025-66842-1
Knihovny.cz E-zdroje
- Publikační typ
- časopisecké články MeSH
Contextualising Arctic warming and sea ice loss requires high-resolution climate proxy archives, which are rare across the high-northern latitudes. Here, we present annually resolved and absolutely dated tree-ring width measurements of living and dry juniper (Juniperus communis) shrubs, as well as herbarium specimens, all from southern Greenland. We develop a continuous chronology for 1526-2023 CE that correlates at 0.67 with mean June‒August temperatures (p < 0.001). We then identify reduced cell wall lignification (i.e., "Blue Rings") during exceptionally cold summers that often occurred after large volcanic eruptions, with Laki in 1783 and Tambora in 1815 CE causing the strongest responses. Our findings at the interface of dendroclimatology and wood anatomy provide a high-resolution paleoclimate record for southern Greenland that places anthropogenic warming in the context of natural climate variability.
Department of Geography Faculty of Science Masaryk University 613 00 Brno Czech Republic
Department of Geography University of Cambridge Cambridge CB2 3EN UK
Global Change Research Institute Czech Academy of Sciences 603 00 Brno Czech Republic
Institute of Geography and Regional Development University of Wroclaw Wroclaw Poland
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