1999/05/07 by Keith R. Briffa, Timothy J. Osborn · 9 citations
Earth and Planetary Sciences · Environmental Science · #Tree-ring climate responses #Plant Water Relations and Carbon Dynamics #Geology and Paleoclimatology Research #Environmental science
paper · doi:10.1126/science.284.5416.926
openalex publication_date 1999/05/07 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/31
Reconstructing past climates is important if we are to distinguish anthropogenic warming from natural variability in the climate system. [Briffa and Osborn][1] discuss a recent study by Mann et al . that has extended their Northern Hemisphere climatic reconstruction to A.D. 1000 and explain why there are large uncertainties in the reconstruction of medieval and earlier temperatures on large spatial scales. Thus, although the 20th century was almost certainly the warmest of the millennium, the amount of anthropogenic warming remains uncertain. [1]: http://www.sciencemag.org/cgi/content/full/284/5416/926