Clim. Past Discuss., 9, 5347-5389, 2013
www.clim-past-discuss.net/9/5347/2013/
doi:10.5194/cpd-9-5347-2013
© Author(s) 2013. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal Climate of the Past (CP). Please refer to the corresponding final paper in CP.
Evaluation of seasonal climates of the Mediterranean and nothern Africa in the CMIP5 simulations
A. Perez-Sanz1,2, G. Li2, P. González-Sampériz1, and S. P. Harrison2,3
1Pyrenean Institute of Ecology, (IPE)-CSIC, Avda. Montañana 1005, 50059 Zaragoza, Spain
2Department of Biological Sciences, Macquarie University, North Ryde, NSW 2109, Australia
3Centre for Past Climates and Department of Geography & Environmental Sciences, School of Archaeology, Geography and Environmental Sciences, (SAGES) University of Reading, Whiteknights, Reading, RG6 6AB, UK

Abstract. We analyze the spatial expression of seasonal climates of the Mediterranean and northern Africa in pre-Industrial (piControl) and mid-Holocene (midHolocene, 6 ka) simulations from the fifth phase of the Coupled Model Intercomparison Project (CMIP5). Modern observations show four distinct precipitation regimes characterized by differences in the seasonal distribution and total amount of precipitation: an equatorial band characterized by a double peak in rainfall, the monsoon zone characterized by summer rainfall, the desert characterized by low seasonality and total precipitation, and the Mediterranean zone characterized by summer drought. Most models correctly simulate the position of the Mediterranean and the equatorial climates in the piControl simulations, but over-estimate the extent of monsoon influence and underestimate the extent of desert. However, most models fail to reproduce the amount of precipitation in each zone. Model biases in the simulated magnitude of precipitation are unrelated to whether the models reproduce the correct spatial patterns of each regime. In the midHolocene, the models simulate a reduction in winter rainfall in the equatorial zone, and a northward expansion of the monsoon with a significant increase in summer and autumn rainfall. Precipitation is slightly increased in the desert, mainly in summer and autumn, with northward expansion of the monsoon. Changes in the Mediterranean are small, although there is an increase in spring precipitation consistent with palaeo-observations of increased growing-season rainfall. Comparison with reconstructions shows that most models under-estimate the mid-Holocene changes in annual precipitation, except in the equatorial zone. Biases in the piControl have only a limited influence on midHolocene anomalies in ocean-atmosphere models; carbon-cycle models show no relationship between piControl bias and midHolocene anomalies. Biases in the prediction of the midHolocene monsoon expansion are unrelated to how well the models simulate changes in Mediterranean climate.

Citation: Perez-Sanz, A., Li, G., González-Sampériz, P., and Harrison, S. P.: Evaluation of seasonal climates of the Mediterranean and nothern Africa in the CMIP5 simulations, Clim. Past Discuss., 9, 5347-5389, doi:10.5194/cpd-9-5347-2013, 2013.
 
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