Climate drivers for peatland palaeoclimate records

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Climate drivers for peatland palaeoclimate records

Please use this identifier to cite or link to this item: http://hdl.handle.net/10036/104986

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Title: Climate drivers for peatland palaeoclimate records
Author: Charman, Dan, J
Barber, Keith E.
Blaauw, Maarten
Langdon, Pete G.
Mauquoy, Dmitri
Daley, Tim J.
Hughes, Paul D.M.
Karofeld, Edgar
Citation: Quaternary Science Reviews, 2009, 28 (19-20): pp. 1811-1819
Publisher: Elsevier Ltd
Journal: Quaternary Science Reviews
Date Issued: 2009-09
URI: http://hdl.handle.net/10036/104986
DOI: 10.1016/j.quascirev.2009.05.013
Links: http://linkinghub.elsevier.com/retrieve/pii/S0277379109001632
Abstract: Reconstruction of hydroclimate variability is an important part of understanding natural climate change on decadal to millennial timescales. Peatland records reconstruct ‘bog surface wetness’ (BSW) changes, but it is unclear whether it is a relative dominance of precipitation or temperature that has driven these variations over Holocene timescales. Previously, correlations with instrumental climate data implied that precipitation is the dominant control. However, a recent chironomid inferred July temperature record suggested temperature changes were synchronous with BSW over the mid-late Holocene. This paper provides new analyses of these data to test competing hypotheses of climate controls on bog surface wetness and discusses some of the distal drivers of large-scale spatial patterns of BSW change. Using statistically based estimates of uncertainty in chronologies and proxy records, we show a correlation between Holocene summer temperature and BSW is plausible, but that chronologies are insufficiently precise to demonstrate this conclusively. Simulated summer moisture deficit changes for the last 6000 years forced by temperature alone are relatively small compared with observations over the 20th century. Instrumental records show that summer moisture deficit provides the best explanatory variable for measured water table changes and is more strongly correlated with precipitation than with temperature in both Estonia and the UK. We conclude that BSW is driven primarily by precipitation, reinforced by temperature, which is negatively correlated with precipitation and therefore usually forces summer moisture deficit in the same direction. In western Europe, BSW records are likely to be forced by changes in the strength and location of westerlies, linked to large-scale North Atlantic ocean and atmospheric circulation.
Type: Article
Description: Reproduced with permission of the publisher. Copyright © 2009 Elsevier Ltd
Keywords: Peatlandbog surface wetnessHoloceneclimate change
ISSN: 02773791


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