Long-term change in summer Arctic air temperatures, as estimated from lake sediments, ice cores and tree rings ('proxy' records)

Direct measurements of temperatures in the Arctic only go back to 1880, but summer temperatures going back 2000 years can be estimated from biological remains found in lake sediments, from gas concentrations in air trapped in shallow ice cores, and from annual growth rings in tree trunks. Analysis of these measurements from across the Arctic shows that a trend of slow summer cooling occurring until around 1800 AD has been dramatically reversed.

2 Files

Download / View Kind Size Lang. Updated
Download: SWIPA Fig 2.1.pdf PDF 954KB English 06/12/2013 13:35:49
Download: SWIPA-Fig 2.1.jpg JPG 561KB English 17/12/2013 15:23:40

Meta Data

Kind Name
Citation AMAP, 2012. Arctic Climate Issues 2011: Changes in Arctic Snow, Water, Ice and Permafrost. SWIPA 2011 Overview Report. Arctic Monitoring and Assessment Programme (AMAP), Oslo. xi + 97pp
Copyright AMAP, 2012
ISBN 978-82-7971-073-8
Published 2012-12-20
Data period/relevance 0-2000
Region arctic