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References

  • Baker, A., and C. Bradley (2010), Modern stalagmite δ18O: Instrumental calibration and forward modelling, Glob. Planet. Change, 71(3–4), 201206.
  • Baker, A., A. Asrat, I. J. Fairchild, M. J. Leng, P. M. Wynn, C. Bryant, D. Genty, and M. Umer (2007), Analysis of the climate signal contained within δ18O and growth rate parameters in two Ethiopian stalagmites, Geochim. Cosmochim. Acta, 71(12), 29752988.
  • Baker, A., C. Bradley, S. J. Phipps, M. Fischer, I. J. Fairchild, L. Fuller, C. Spötl, and C. Azcurra (2012), Millennial-length forward models and pseudoproxies of stalagmite δ18O: An example from NW Scotland, Clim. Past, 8, 11531167.
  • Bradley, C., A. Baker, C. N. Jex, and M. J. Leng (2010), Hydrological uncertainties in the modelling of cave drip-water δ18O and the implications for stalagmite palaeoclimate reconstructions, Quaternary Sci. Rev., 29(17–18), 22012214.
  • Cai, B., N. Pumijumnong, M. Tan, C. Muangsong, X. Kong, X. Jiang, and S. Nan (2010), Effects of intraseasonal variation of summer monsoon rainfall on stable isotope and growth rate of a stalagmite from northwestern Thailand, J. Geophys. Res., 115, D21104, doi:10.1029/2009JD013378.
  • Jex, C. N., A. Baker, I. J. Fairchild, W. J. Eastwood, M. J. Leng, H. J. Sloane, L. Thomas, and E. Bekaroğlu (2010), Calibration of speleothem δ18O with instrumental climate records from Turkey, Glob. Planet. Change, 71(3–4), 207217.
  • Jex, C. N., A. Baker, J. M. Eden, W. J. Eastwood, I. J. Fairchild, M. J. Leng, L. Thomas, and H. J. Sloane (2011), A 500 yr speleothem-derived reconstruction of late autumn–winter precipitation, northeast Turkey, Quaternary Res., 75(3), 399405.
  • Kim, S.-T., and J. R. O'Neil (1997), Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates, Geochim. Cosmochim. Acta, 61(16), 34613475.
  • Kutiel, H. (2011), A review on the impact of the North Sea–Caspian Pattern (NCP) on temperature and precipitation regimes in the Middle East, in Survival and Sustainability, edited by H. Gökçekus, U. Türker, and J. W. LaMoreaux, pp. 13011312, Springer, Berlin, Heidelberg.
  • Kutiel, H., and Y. Benaroch (2002), North Sea-Caspian Pattern (NCP)—An upper level atmospheric teleconnection affecting the Eastern Mediterranean: Identification and definition, Theor. Appl. Climatol., 71(1), 1728.
  • Kutiel, H., P. Maheras, M. Türkeş, and S. Paz (2002), North Sea–Caspian Pattern (NCP)—An upper level atmospheric teleconnection affecting the eastern Mediterranean—Implications on the regional climate, Theor. Appl. Climatol., 72(3), 173192.
  • Lohmann, G., A. Wackerbarth, P. M. Langebroek, M. Werner, J. Fohlmeister, D. Scholz, and A. Mangini (2013), Simulated European stalagmite record and its relation to a quasi-decadal climate mode, Clim. Past, 9(1), 8998.
  • Mattey, D., D. Lowry, J. Duffet, R. Fisher, E. Hodge, and S. Frisia (2008), A 53 year seasonally resolved oxygen and carbon isotope record from a modern Gibraltar speleothem: Reconstructed drip water and relationship to local precipitation, Earth Planet. Sci. Lett., 269(1–2), 8095.
  • van Oldenborgh, G. J., M. A. Balmaseda, L. Ferranti, T. N. Stockdale, and D. L. T. Anderson (2005), Evaluation of atmospheric fields from the ECMWF seasonal forecasts over a 15-year period, J. Climate, 18(16), 32503269.
  • Phipps, S. J., L. D. Rotstayn, H. B. Gordon, J. L. Roberts, A. C. Hirst, and W. F. Budd (2011), The CSIRO Mk3L climate system model version 1.0—Part 1: Description and evaluation, Geosci. Model Dev., 4, 483509.
  • Phipps, S. J., L. D. Rotstayn, H. B. Gordon, J. L. Roberts, A. C. Hirst, and W. F. Budd (2012), The CSIRO Mk3L climate system model version 1.0—Part 2: Response to external forcings, Geosci. Model Dev., 5, 649682.
  • Rowe, P. J., J. E. Mason, J. E. Andrews, A. D. Marca, L. Thomas, P. van Calsteren, C. N. Jex, H. B. Vonhof, and S. Al-Omari (2012), Speleothem isotopic evidence of winter rainfall variability in northeast Turkey between 77 and 6 ka, Quaternary Sci. Rev., 45, 6072.
  • Sturm, C., Q. Zhang, and D. Noone (2010), An introduction to stable water isotopes in climate models: benefits of forward proxy modelling for paleoclimatology, Clim. Past, 6(1), 115129.
  • Tatli, H. (2007), Synchronization between the North Sea–Caspian pattern (NCP) and surface air temperatures in NCEP, Int. J. Climatol., 27(9), 11711187.
  • Türkeş, M., and E. Erlat (2003), Precipitation changes and variability in Turkey linked to the North Atlantic oscillation during the period 1930–2000, Int. J. Climatol., 23(14), 17711796.
  • Türkeş, M., and E. Erlat (2005), Climatological responses of winter precipitation in Turkey to variability of the North Atlantic Oscillation during the period 1930–2001, Theor. Appl. Climatol., 81(1), 4569.
  • Uppala, S. M. et al. (2005), The ERA-40 re-analysis, Quart. J. Roy. Meteor. Soc., 131(612), 29613012.
  • Wackerbarth, A., D. Scholz, J. Fohlmeister, and A. Mangini (2010), Modelling the δ18O value of cave drip water and speleothem calcite, Earth Planet. Sci. Lett., 299(3–4), 387397.
  • Wackerbarth, A., P. M. Langebroek, M. Werner, G. Lohmann, S. Riechelmann, A. Borsato, and A. Mangini (2012), Simulated oxygen isotopes in cave drip water and speleothem calcite in European caves, Clim. Past, 8(6), 17811799.
  • Yadava, M. G., R. Ramesh, and G. B. Pant (2004), Past monsoon rainfall variations in peninsular India recorded in a 331-year-old speleothem, Holocene, 14(4), 517524.