Globally resolved surface temperatures since the Last Glacial Maximum

2021/11/10 by Matthew B. Osman, Matthew Osman, Jessica E. Tierney +5 · 1 voice · 24 citations
Earth and Planetary Sciences · Environmental Science · #Geology and Paleoclimatology Research #Isotope Analysis in Ecology #Tree-ring climate responses

paper · doi:10.1038/s41586-021-03984-4

crossref issued 2021/11/10 · crossref published 2021/11/10 · crossref published-online 2021/11/10 · openalex publication_date 2021/11/10 · crossref created 2021/11/10 · crossref published-print 2021/11/11 · crossref deposited 2023/11/12 · openalex created_date 2025/10/10 · crossref indexed 2026/07/24 · openalex updated_date 2026/07/29

Citations

• Long-Term Variations of Daily Insolation and Quaternary Climatic Changes
• On the Structure and Origin of Major Glaciation Cycles 1. Linear Responses to Milankovitch Forcing
• Law Dome CO2, CH4 and N2O ice core records extended to 2000 years BP
• IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP
• Glacial cooling and climate sensitivity revisited
• Seasonal origin of the thermal maxima at the Holocene and the last interglacial
• IntCal09 and Marine09 Radiocarbon Age Calibration Curves, 0–50,000 Years cal BP

Cited by

• Global variability in LGM cooling amongst paleoclimate datasets affects biome reconstructions in mountains
• A 485-million-year history of Earth’s surface temperature
• Unravelling the tree cover dynamics over the last 20 000 years on the Northern Hemisphere
• Global and regional temperature change over the past 4.5 million years
• Temperature-dependent feedbacks drive the pattern of Antarctic temperature change
• We Are in the Anthropocene—Now What?
• Safe and just Earth system boundaries
• Earth beyond six of nine planetary boundaries
• Exceeding 1.5°C global warming could trigger multiple climate tipping points
• Phylogenetic relationships and modeling distributions of the monotypic genus Dolichopetalum (Apocynaceae): Implications for conservation of unique biodiversity in Asian subtropical karst areas
• Global warming in the pipeline
• Two decades of climate tipping points research: Progress and outlook
• Southern Ocean seabird population shifts over the Holocene revealed by peat sequestration of mercury from guano
• Tropical response to ocean circulation slowdown raises future drought risk
• Phanerozoic orbital-scale glacio-eustatic variability
• Winter is coming: Interactions of multiple stressors in winter and implications for the natural world
• Late mid-Holocene cooling indicated by the Chibuzhang Co record in the central Tibetan Plateau
• Local hydroclimate alters interpretation of speleothem δ18O records
• Mid‐Holocene drying of K'gari lakes (subtropical eastern Australia) necessitates re‐evaluation of the El Niño–Southern Oscillation climate links and future drying risk
• Climate changes revealed from the aeolian sediments in the Menyuan Basin, northeastern Qinghai-Tibet Plateau
• Testing the reliability of global surface temperature reconstructions of the Last Glacial Cycle with pseudo-proxy experiments
• Temperature changes during the last deglaciation and early Holocene in southwest China
• Isotopic evidence for elevated photorespiration during the last glacial period
• The planetary commons: A new paradigm for safeguarding Earth-regulating systems in the Anthropocene

Discussions

• For much of the Holocene global average temperatures were not greatly different from those up to the mid 20th century, but were not as warm as those we have experienced more recently. Graph below is [bsky, 1 points, 1 comments]