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The Spatial Extent of 20th-Century Warmth in the Context of the Past 1200 Years

2006/02/09 by Timothy J. Osborn, Keith R. Briffa · 14 citations
Earth and Planetary Sciences · Environmental Science · #Archaeology #Art #Climate variability and models #Climatology #Context (archaeology) #Geography #Geology #Geology and Paleoclimatology Research #History #Little ice age #Northern Hemisphere #Period (music) #Physical geography #Proxy (statistics) #Statistics #Tree-ring climate responses

paper · doi:10.1126/science.1120514

openalex publication_date 2006/02/09 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/23

Abstract

Periods of widespread warmth or cold are identified by positive or negative deviations that are synchronous across a number of temperature-sensitive proxy records drawn from the Northern Hemisphere. The most significant and longest duration feature during the last 1200 years is the geographical extent of warmth in the middle to late 20th century. Positive anomalies during 890 to 1170 and negative anomalies during 1580 to 1850 are consistent with the concepts of a Medieval Warm Period and a Little Ice Age, but comparison with instrumental temperatures shows the spatial extent of recent warmth to be of greater significance than that during the medieval period.

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