MULTI-ARCHIVE TEMPERATURE RECONSTRUCTION OF THE RUSSIAN ARCTIC FOR THE PAST TWO MILLENNIA

We present a multi-archival mean annual quantitative temperature reconstruction for Northeastern Europe covering the period of the past two millennia based on tree-ring, pollen, and historical data. This reconstruction was developed primarily to build up a comparative chronology of climatic and hist...

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Bibliographic Details
Published in:GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
Main Authors: Vladimir Klimenko, Vladimir Matskovsky, Dittmar Dahlmann
Format: Article in Journal/Newspaper
Language:English
Published: Lomonosov Moscow State University 2014
Subjects:
climate change
arctic
palaeogeography
temperature reconstruction
multi-proxy
historical climatology
Geography (General)
G1-922
Arctic
Climate change
Online Access:https://doi.org/10.24057/2071-9388-2014-7-1-16-29
https://doaj.org/article/c3ec0e44dae14f17839934a66149db50
Description
Summary:We present a multi-archival mean annual quantitative temperature reconstruction for Northeastern Europe covering the period of the past two millennia based on tree-ring, pollen, and historical data. This reconstruction was developed primarily to build up a comparative chronology of climatic and historical events in the study region. Five different calibration and verification approaches were used. A comparison of mean decadal temperature reconstruction for Northeastern Europe with those for larger regions and the Hemisphere shows that larger climatic events were visible both in the whole Northern Hemisphere and its separate regions. Less significant climatic events on a regional level may differ considerably from the overall climate signature on the hemispheric level. Highest pre-industrial mean annual temperatures in AD 981-990 were 1,0°C warmer and lowest in AD 1811-1820 were 1,3°C colder than average in AD 1951-1980. The new reconstruction shows much higher degree of variability as compared to Panarctic and hemispheric reconstructions.

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