Accessibility navigation

Underlying causes of Eurasian mid-continental aridity in simulations of mid-Holocene climate

Bartlein, P. J., Harrison, S. P. and Izumi, K. (2017) Underlying causes of Eurasian mid-continental aridity in simulations of mid-Holocene climate. Geophysical Research Letters, 44 (17). pp. 9020-9028. ISSN 0094-8276

Text (Open Access) - Published Version
· Available under License Creative Commons Attribution.
· Please see our End User Agreement before downloading.

[img] Text - Accepted Version
· Restricted to Repository staff only
· Available under License Creative Commons Attribution.


It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing.

To link to this item DOI: 10.1002/2017GL074476


The CMIP5/PMIP3 mid-Holocene simulations show drier conditions in the Eurasian mid-continent and a significant increase in summer temperature; in contrast, paleoenvironmental data (including lake level, vegetation and isotope records, and aeolian deposits) and quantitative climate reconstructions show that the mid-continental extratropics were wetter than today and summers were cooler (Harrison et al., 2015). Eurasian mid-continental aridity and warming has been a persistent feature of model simulations, already present in atmosphere-only simulations (Yu & Harrison, 1996) and appearing more strongly in coupled ocean-atmosphere simulations (e.g. Braconnot et al., 2007b; Wohlfahrt et al., 2008; Harrison et al., 2015) and further exacerbated by vegetation feedback (Wohlfarht et al., 2004). The consistency among multiple lines of paleoenvironmental evidence makes it unlikely that the mismatch reflects misinterpretation of the data. Regional temperature biases in the CMIP5 20th century simulations have been linked to biases in surface energy and water balances, with over- or under-prediction of moisture fluxes and evapotranspiration leading to cold and warm temperature biases respectively (Mueller & Seneviratne, 2014). This suggests that discrepancies in the simulation of mid-Holocene climates might have a similar cause. In this paper, we investigate the processes involved in mid-continental climate changes in the CMIP5/PMIP3 simulations in order to identify the underlying cause of the mismatch with observations.

Item Type:Article
Divisions:Science > School of Archaeology, Geography and Environmental Science > Department of Geography and Environmental Science
Interdisciplinary centres and themes > Centre for Past Climate Change
ID Code:72170
Publisher:American Geophysical Union


Downloads per month over past year

University Staff: Request a correction | Centaur Editors: Update this record

Page navigation