2013/03/07 by Shaun A. Marcott, Jeremy D. Shakun, Peter U. Clark +1 · 2 citations
Earth and Planetary Sciences · #Geology and Paleoclimatology Research #Tree-ring climate responses #Archaeology and ancient environmental studies #Deglaciation #Holocene #Proxy (statistics) #Global warming #Climatology #Physical geography #Climate change #Little ice age #Paleoclimatology #Surface air temperature #Global temperature #Global cooling #Geology #Oceanography #Environmental science #Geography
paper · doi:10.1126/science.1228026
openalex publication_date 2013/03/07 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/29
Surface temperature reconstructions of the past 1500 years suggest that recent warming is unprecedented in that time. Here we provide a broader perspective by reconstructing regional and global temperature anomalies for the past 11,300 years from 73 globally distributed records. Early Holocene (10,000 to 5000 years ago) warmth is followed by ~0.7°C cooling through the middle to late Holocene (<5000 years ago), culminating in the coolest temperatures of the Holocene during the Little Ice Age, about 200 years ago. This cooling is largely associated with ~2°C change in the North Atlantic. Current global temperatures of the past decade have not yet exceeded peak interglacial values but are warmer than during ~75% of the Holocene temperature history. Intergovernmental Panel on Climate Change model projections for 2100 exceed the full distribution of Holocene temperature under all plausible greenhouse gas emission scenarios.