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3 - Past climates of the Middle East

from Part I - Past, present and future climate

Published online by Cambridge University Press:  26 April 2011

David Brayshaw
Affiliation:
University of Reading
Emily Black
Affiliation:
University of Reading
Brian Hoskins
Affiliation:
University of Reading
Julia Slingo
Affiliation:
University of Reading
Steven Mithen
Affiliation:
University of Reading
Emily Black
Affiliation:
University of Reading
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Summary

ABSTRACT

In this chapter, we develop an improved understanding of the Mediterranean's past climate through a series of ‘time-slice’ climate integrations relating to the past 12,000 years, performed using a version of the Met Office Hadley Centre's global climate model (HadSM3). The output is dynamically downscaled using a regional version of the same model to offer unprecedented spatial detail over the Mediterranean. Changes in seasonal surface air temperatures and precipitation are discussed at both global and regional scales along with their underlying physical drivers.

In the experiments the Mediterranean experiences more precipitation in the early Holocene than the late Holocene, although the difference is not uniform across the eastern Mediterranean. The results suggest that there may have been a relatively strong reduction in precipitation over the eastern Mediterranean coast during the period around 6–10 thousand years before present (kaBP). The early Holocene also shows a stronger seasonal cycle of temperature throughout the Northern Hemisphere but, over the northeast Mediterranean, this is mitigated by the influence of milder maritime air carried inland from the coast.

INTRODUCTION

Understanding the changes in the Mediterranean climate during the Holocene period is a challenging problem, but one that is critical to interpreting long-term change in human settlement. The region at present displays marked seasonality with dry, hot summers and cool, wet winters.

Type
Chapter
Information
Water, Life and Civilisation
Climate, Environment and Society in the Jordan Valley
, pp. 25 - 50
Publisher: Cambridge University Press
Print publication year: 2011

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References

Arz, H. W., Lamy, F., Patzold, J., Muller, P. J. and Prins, M. (2003) Mediterranean moisture source for an Early-Holocene humid period in the Northern Red Sea. Science 300: 118–121.CrossRefGoogle ScholarPubMed
Barlow, M., Wheeler, M., Lyon, B. and Cullen, H. (2005) Modulation of daily precipitation over Southwest Asia by the Madden-Julian Oscillation. Monthly Weather Review 133: 3579–3594.CrossRefGoogle Scholar
Berger, A.L. (1978) Long term variations of daily insolation and Quaternary climatic changes. Journal of the Atmospheric Sciences 35: 2362–2367.2.0.CO;2>CrossRefGoogle Scholar
Black, E. (2009) The impact of climate change on daily precipitation statistics for Jordan and Israel. Atmospheric Science Letters 10: 192–200.CrossRefGoogle Scholar
Bonfils, C., Noblet-Ducoudre, N., Guiot, J. and Bartlein, P. (2004) Some mechanisms of Mid-Holocene climate change in Europe, inferred from comparing PMIP models to data. Climate Dynamics 23: 79–98.CrossRefGoogle Scholar
Braconnot, P., Otto-Bliesner, B., Harrison, S.et al. (2007) Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum – Part 1: experiments and large-scale features. Climate of the Past 3: 261–277.CrossRefGoogle Scholar
Brayshaw, D. J., Hoskins, B. and Blackburn, M. (2008) The storm track response to idealised SST perturbations in an aquaplanet GCM. Journal of the Atmospheric Sciences 65: 2842–2860.CrossRefGoogle Scholar
Brayshaw, D. J., Hoskins, B. and Blackburn, M. (2009) The basic ingredients of the North Atlantic storm track. Part I: Land–sea contrast and orography. Journal of the Atmospheric Sciences 66: 2539–2558.CrossRefGoogle Scholar
Brayshaw, D., Hoskins, B. and Black, E. (2010) Some physical drivers of changes in the winter storm tracks over the North Atlantic and Mediterranean during the Holocene. Philosophical Transactions of the Royal Society A, 368: 5185–5223.CrossRefGoogle ScholarPubMed
Cheddadi, R., Yu, G., Guiot, J., Harrison, S. and Prentice, I. C. (1997) The climate of Europe 6000 years ago. Climate Dynamics 13: 1–9.CrossRefGoogle Scholar
Claussen, M., Kubatzki, C., Brovkin, V.et al. (1999) Simulation of an abrupt change in Saharan vegetation in the Mid-Holocene. Geophysical Research Letters 26: 2037–2040.CrossRefGoogle Scholar
Crossley, J. F. and Roberts, D. L. (1995) The Thermodynamic/Dynamic Sea Ice Model. Unified Model Documentation Paper 45 Met Office.
Dai, A. G., Hu, A., Meehl, G. A., Washington, W. M. and Strand, W. G. (2005) Atlantic thermohaline circulation in a coupled general circulation model: Unforced variations versus forced changes. Journal of Climate 18: 3270–3293.CrossRefGoogle Scholar
Davis, B. A. S., Brewer, S., Stevenson, A. C.et al. (2003) The temperature of Europe during the Holocene reconstructed from pollen data. Quaternary Science Reviews 22: 1701–1716.CrossRefGoogle Scholar
Drake, N. and Bristow, C. (2006) Shorelines in the Sahara: geomorphological evidence for an enhanced monsoon from palaeolake Megachad. The Holocene 16: 901–911.CrossRefGoogle Scholar
Edmon, H. J., Hoskins, B. and McIntyre, M. E. (1980) Eliassen-Palm cross sections for the troposphere. Journal of the Atmospheric Sciences 37: 2600–2616.2.0.CO;2>CrossRefGoogle Scholar
Gladstone, R. M., Ross, I., Valdes, P. J.et al. (2005) Mid-Holocene NAO: A PMIP2 model intercomparison. Geophysical Research Letters 32: L16707, DOI:10.1029/2005GL023596.CrossRefGoogle Scholar
Hegerl, G. C., Zwiers, F., Braconnot, P.et al. (2007) Understanding and attributing climate change. In Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. Solomon, S., Qin, D., Manning, M.et al. Cambridge and New York: Cambridge University Press.Google Scholar
Hewitt, C. D., Senior, C. A. and Mitchell, J. F. B. (2001) The impact of dynamic sea-ice on the climatology and climate sensitivity of a GCM: a study of past, present, and future climates. Climate Dynamics 17: 655–668.CrossRefGoogle Scholar
Hoskins, B. J. and Hodges, K. I. (2002) New perspectives on the Northern Hemisphere winter storm tracks. Journal of the Atmospheric Sciences 59: 1041–1061.2.0.CO;2>CrossRefGoogle Scholar
Hoskins, B. J. and Valdes, P. J. (1990) On the existence of storm-tracks. Journal of the Atmospheric Sciences 47: 1854–1864.2.0.CO;2>CrossRefGoogle Scholar
Hoskins, B. J., James, I. N. and White, G. H. (1983) The shape, propagation and mean-flow interaction of large-scale weather systems. Journal of the Atmospheric Sciences 40: 1595–1612.2.0.CO;2>CrossRefGoogle Scholar
Jansen, E., Overpeck, J., Briffa, K. R.et al. (2007) Palaeoclimate. In Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. Solomon, S., Qin, D., Manning, M.et al. Cambridge and New York: Cambridge University Press.Google Scholar
Jolly, D., Prentice, I. C., Bonnefille, R.et al. (1998) Biome reconstruction from pollen and plant macrofossil data for Africa and the Arabian peninsula at 0 and 6000 years. Journal of Biogeography 25: 1007–1027.CrossRefGoogle Scholar
Meehl, G. A., Stocker, T. F., Collins, W.et al. (2007) Global climate projections. In Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. Solomon, S., Qin, D., Manning, M.et al. Cambridge and New York: Cambridge University Press.Google Scholar
Otto-Bliesner, B. L., Brady, E. C., Clauzet, G.et al. (2006) Last Glacial Maximum and Holocene climate in CCSM3. Journal of Climate 19: 2526–2544.CrossRefGoogle Scholar
Peltier, W. R. (1994) Ice-age paleotopography. Science 265: 195–201.CrossRefGoogle ScholarPubMed
Pope, V. D., Gallani, M. L., Rowntree, P. R. and Stratton, R. A. (2000) The impact of new physical parametrizations in the Hadley Centre climate model: HadAM3. Climate Dynamics 16: 123–146.CrossRefGoogle Scholar
Rimbu, N., Lohmann, G., Kim, J. H., Arz, H. W. and Schneider, R. (2003) Arctic/North Atlantic Oscillation signature in Holocene sea surface temperature trends as obtained from alkenone data. Geophysical Research Letters 30: DOI 10.1029/2002GL016570.CrossRefGoogle Scholar
Rimbu, N., Lohmann, G., Lorenz, S. J., Kim, J. H. and Schneider, R. R. (2004) Holocene climate variability as derived from alkenone sea surface temperature and coupled ocean-atmosphere model experiments. Climate Dynamics 23: 215–227.CrossRefGoogle Scholar
Rodwell, M. J. and Hoskins, B. J. (2001) Subtropical anticyclones and summer monsoons. Journal of Climate 14: 3192–3211.2.0.CO;2>CrossRefGoogle Scholar
Rohling, E. J. and Rijk, S. (1999) Holocene Climate Optimum and Last Glacial Maximum in the Mediterranean: the marine oxygen isotope record. Marine Geology 153: 57–75.CrossRefGoogle Scholar
Rudolf, B., Hauschild, H., Rueth, W. and Schneider, U. (1994) Terrestrial precipitation analysis: Operational method and required density of point measurements. In Global Precipitations and Climate Change, ed. Desbois, M. and Desalmond, F.. Berlin: Springer-Verlag pp. 173–186.CrossRefGoogle Scholar
Stratton, R. A. (1994) Report on aspects of variability in high-resolution versions of HadAM3. Hadley Centre Technical Note 53.Google Scholar
Taylor, K. E., Williamson, D. and Zwiers, F. (2000) The sea surface temperature and sea-ice concentration boundary conditions for AMIP II simulationsPCMDI Report 60. California: Lawrence Livermore National Laboratory Program for Climate Model Diagnosis and Intercomparison.Google Scholar
Texier, D., Noblet, N. and Braconnot, P. (2000) Sensitivity of the African and Asian monsoons to Mid-Holocene insolation and data-inferred surface changes. Journal of Climate 13: 164–181.2.0.CO;2>CrossRefGoogle Scholar
Trenberth, K. E., Jones, P. D., Ambenje, P.et al. (2007) Observations: surface and atmospheric climate change. In Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, ed. Solomon, S., Qin, D., Manning, M.et al. Cambridge and New York: Cambridge University Press pp. 433–497.Google Scholar
Trigo, I. F., Davies, T. D. and Bigg, G. R. (1999) Objective climatology of cyclones in the Mediterranean region. Journal of Climate 12: 1685–1696.2.0.CO;2>CrossRefGoogle Scholar
Uppala, S. M., Kallberg, P. W., Simmons, A. J.et al. (2005) The ERA-40 re-analysis. Quarterly Journal of the Royal Meteorological Society 131: 2961–3012.CrossRefGoogle Scholar
Wanner, H., Beer, J., Butikofer, J.et al. (2008) Mid- to late Holocene climate change: an overview. Quaternary Science Reviews 27: 1791–1828.CrossRefGoogle Scholar
Wilks, D. S. (1995) Statistical Methods in the Atmospheric Sciences: An Introduction. San Diego: Academic Press.Google Scholar
Wood, R. A., Keen, A. B., Mitchell, J. F. B. and Gregory, J. M. (1999) Changing spatial structure of the thermohaline circulation in response to atmospheric CO2 forcing in a climate model. Nature 399: 572–575.CrossRefGoogle Scholar
Yin, J. H. (2005) A consistent poleward shift of the storm tracks in simulations of 21st century climate. Geophysical Research Letters 32: DOI 10.1029/2005GL023684.CrossRefGoogle Scholar

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