SEARCH

SEARCH BY CITATION

References

  • Berger, A. L. (1978), Long-term variations of caloric insolation resulting from the Earth's orbital elements, Quat. Res., 9, 139167.
  • Bonfils, C., N. de Noblet, J. Guiot, and P. Bartlein (2004), Some mechanisms of mid-Holocene climate change in Europe, inferred from comparing PMIP models to data, Clim. Dyn., 23, 7998.
  • Braconnot, P., O. Marti, S. Joussaume, and Y. Leclainche (2000), Ocean feedback in response to 6 kyr BP insolation, J. Clim., 13, 15371553.
  • Braconnot, P., et al. (2007a), Results of PMIP2 coupled simulations of the mid-Holocene and last glacial maximum, Part 1: Experiments and large-scale features, Clim. Past, 3, 261277.
  • Braconnot, P., et al. (2007b), Results of PMIP2 coupled simulations of the mid-Holocene and last glacial maximum, Part 2: Feedbacks with emphasis on the location of the ITCZ and mid- and high latitudes heat budget, Clim. Past, 3, 279296.
  • Chen, L. X., Q. G. Zhu, H. B. Luo, J. H. He, M. Dong, and Z. Q. Feng (1991), East Asian Monsoon, pp. 1362, Meteorol. Press, Beijing.
  • Claussen, M., and V. Gayler (1997), The greening of the Sahara during the mid-Holocene: Results of an interactive atmosphere-biome model, Global Ecol. Biogeogr. Lett., 6, 369377.
  • Coe, M. T., and S. P. Harrison (2002), The water balance of northern Africa during the mid-Holocene: An evaluation of the 6 ka BP PMIP simulations, Clim. Dyn., 19, 155166.
  • Collins, W. D., et al. (2006a), The Community Climate System Model version 3 (CCSM3), J. Clim., 19, 21222143.
  • Collins, W. D., et al. (2006b), The formulation and atmospheric simulation of the Community Atmosphere Model version 3 (CAM3), J. Clim., 19, 21442161.
  • Dallmeyer, A., M. Claussen, and J. Otto (2010), Contribution of oceanic and vegetation feedbacks to Holocene climate change in monsoonal Asia, Clim. Past, 6, 195218.
  • de Noblet, N., P. Braconnot, S. Joussaume, and V. Masson (1996), Sensitivity of simulated Asian and African summer monsoons to orbitally induced variations in insolation 126, 115 and 6 kBP, Clim. Dyn., 12, 589603.
  • Gent, P. R., F. O. Bryan, G. Danabasoglu, K. Lindsay, D. Tsumune, M. W. Hecht, and S. C. Doney (2006), Ocean chlorofluorocarbon and heat uptake during the twentieth century in the CCSM3, J. Clim., 19, 23662381.
  • Hall, N. M. J., and P. J. Valdes (1997), A GCM simulation 6000 years ago, J. Clim., 10, 317.
  • Harrison, S. P., et al. (1998), Intercomparison of simulated global vegetation distributions in response to 6 kyr BP orbital forcing, J. Clim., 11, 27212742.
  • He, J. H., J. H. Ju, Z. P. Wen, J. M. Lü, and Q. H. Jin (2007), A review of recent advances in research on Asian monsoon in China, Adv. Atmos. Sci., 24, 972992.
  • Hewitt, C. D., and J. F. B. Mitchell (1998), A fully coupled GCM simulation of the mid-Holocene, Geophys. Res. Lett., 25(3), 361364, doi:10.1029/97GL03721.
  • Jolly, D., et al. (1998), Biome reconstruction from pollen and plant macrofossil data for Africa and the Arabian Peninsula at 0 and 6000 years, J. Biogeogr., 25, 10071027.
  • Joussaume, S., et al. (1999), Monsoon changes for 6000 years ago: results of 18 simulations from the Paleoclimate Modeling Intercomparison Project (PMIP), Geophys. Res. Lett., 26(7), 859862, doi:10.1029/1999GL900126.
  • Kohfeld, K. E., and S. P. Harrison (2000), How well can we simulate past climates? Evaluating the models using global palaeoenvironmental datasets, Quat. Sci. Rev., 19, 321346.
  • Kutzbach, J. E., and P. J. Guetter (1986), The influence of changing orbital parameters and surface boundary conditions on climate simulations for the past 18,000 years, J. Atmos. Sci., 43, 17261759.
  • Kutzbach, J. E., and Z. Liu (1997), Response of the African monsoon to orbital forcing and ocean feedbacks in the middle Holocene, Science, 278, 440443.
  • Kutzbach, J. E., G. Bonan, J. Foley, and S. P. Harrison (1996), Vegetation and soil feedbacks on the response of the African monsoon to orbital forcing in the early to middle Holocene, Nature, 384, 623626.
  • Levis, S., G. B. Bonan, and C. Bonfils (2004), Soil feedback drives the mid-Holocene North African monsoon northward in fully coupled CCSM2 simulations with a dynamic vegetation model, Clim. Dyn., 23, 791802.
  • Liu, Z., E. C. Brady, and J. Lynch-Stieglitz (2003a), Global ocean response to orbital forcing in the Holocene, Paleoceanography, 18(2), 1041, doi:10.1029/2002PA000819.
  • Liu, Z., B. Otto-Bliesner, J. Kutzbach, L. Li, and C. Shields (2003b), Coupled climate simulation of the evolution of global monsoons in the Holocene, J. Clim., 16, 24722490.
  • Liu, Z., S. P. Harrison, J. Kutzbach, and B. Otto-Bliesner (2004), Global monsoons in the mid-Holocene and oceanic feedback, Clim. Dyn., 22, 157182.
  • Marzin, C., and P. Braconnot (2009a), Variations of Indian and African monsoons induced by insolation changes at 6 and 9.5 kyr BP, Clim. Dyn., 33, 215231.
  • Marzin, C., and P. Braconnot (2009b), The role of the ocean feedback on Asian and African monsoon variations at 6 kyr and 9.5 kyr BP, C. R. Geosci., 341, 643655.
  • Nan, S., P. Zhao, S. Yang, and J. Chen (2009), Springtime tropospheric temperature over the Tibetan Plateau and evolutions of the tropical Pacific SST, J. Geophys. Res., 114, D10104, doi:10.1029/2008JD011559.
  • Ni, J., Y. Ge, S. P. Harrison, and I. C. Prentice (2010), Palaeovegetation in China during the late Quaternary: Biome reconstructions based on a global scheme of plant functional types, Palaeogeogr. Palaeoclimatol. Palaeoecol., 289, 4461.
  • Ohgaito, R., and A. Abe-Ouchi (2007), The role of ocean thermodynamics and dynamics in Asian summer monsoon changes during the mid-Holocene, Clim. Dyn., 29, 3950.
  • Otto-Bliesner, B. L., E. C. Brady, G. Clauzet, R. Tomas, S. Levis, and Z. Kothavala (2006), Last glacial maximum and Holocene climate in CCSM3, J. Clim., 19, 25262544.
  • Prentice, I. C., D. Jolly, and Biome 6000 Participants (2000), Mid-Holocene and glacial-maximum vegetation geography of the northern continents and Africa, J. Biogeogr., 27, 507519.
  • Renssen, H., H. Goosse, T. Fichefet, V. Brovkin, E. Driesschaert, and F. Wolk (2005), Simulating the Holocene climate evolution at northern high latitudes using a coupled atmosphere-sea ice-ocean-vegetation model, Clim. Dyn., 24, 2343.
  • Uppala, S. M., et al. (2005), The ERA-40 reanalysis, Q. J. R. Meteorol. Soc., 131, 29613012.
  • Voss, R., and U. Mikolajewicz (2001), The climate of 6000 years BP in near-equilibrium simulations with a coupled AOGCM, Geophys. Res. Lett., 28(11), 22132216, doi:10.1029/2000GL012498.
  • Wang, H. J. (1999), Role of vegetation and soil in the Holocene megathermal climate over China, J. Geophys. Res., 104(D8), 93619367, doi:10.1029/1999JD900049.
  • Wang, H. J. (2000), The seasonal climate and low frequency oscillation in the simulated mid-Holocene megathermal climate, Adv. Atmos. Sci., 17, 445457.
  • Wang, H. J. (2002), The mid-Holocene climate simulated by a grid-point AGCM coupled with a biome model, Adv. Atmos. Sci., 19, 205218.
  • Wang, T., H. J. Wang, and D. B. Jiang (2010), Mid-Holocene East Asian summer climate as simulated by the PMIP2 models, Palaeogeogr. Palaeoclimatol. Palaeoecol., 288, 93102.
  • Wang, Y., M. Notaro1, Z. Liu, R. Gallimore, S. Levis, and J. E. Kutzbach (2008), Detecting vegetation-precipitation feedbacks in mid-Holocene North Africa from two climate models, Clim. Past, 4, 5967.
  • Wanner, H., et al. (2008), Mid- to late Holocene climate change: an overview, Quat. Sci. Rev., 27, 17911828.
  • Wohlfahrt, J., S. P. Harrison, and P. Braconnot (2004), Synergistic feedbacks between ocean and vegetation on mid- and high-latitude climates during the mid-Holocene, Clim. Dyn., 22, 223238.
  • Wohlfahrt, J., S. P. Harrison, P. Braconnot, C. D. Hewitt, A. Kitoh, U. Mikolajewicz, B. L. Otto-Bliesner, and S. L. Weber (2008), Evaluation of coupled ocean-atmosphere simulations of the mid-Holocene using paleovegetation data from the northern hemisphere extratropics, Clim. Dyn., 31, 871890.
  • Wu, Y. H., A. Lücke, Z. D. Jin, S. M. Wang, G. H. Schleser, R. W. Battarbee, and W. L. Xia (2006), Holocene climate development on the central Tibetan Plateau: A sedimentary record from Cuoe Lake, Palaeogeogr. Palaeoclimatol. Palaeoecol., 234, 328340.
  • Xue, B., and G. Yu (2000), Changes of atmospheric circulation since the last interstadial as indicated by the lake-status record in China, Acta Geol. Sin., 74, 836845.
  • Yu, G., and S. P. Harrison (1996), An evaluation of the simulated water balance of Eurasia and northern Africa at 6000 y BP using lake status data, Clim. Dyn., 12, 723735.
  • Yu, G., I. C. Prentice, S. P. Harrison, and X. Sun (1998), Pollen-based biome reconstructions for China at 0 and 6000 years, J. Biogeogr., 25, 10551069.
  • Yu, G., et al. (2000), Palaeovegetation of China: a pollen data-based synthesis for the mid mid-Holocene and last glacial maximum, J. Biogeogr., 27, 635664.
  • Yu, G., B. Xue, J. Liu, X. Chen, and Y. Q. Zheng (2001), Lakes evolution in China and paleoclimatic dynamics, Meteorolog. Press, Beijing, pp. 1196.
  • Zhao, P., Y. N. Zhu, and R. H. Zhang (2007), An Asian-Pacific teleconnection in summer tropospheric temperature and associated Asian climate variability, Clim. Dyn., 29, 293303.
  • Zhao, P., J. M. Chen, D. Xiao, S. L. Nan, Y. Zou, and B. T. Zhou (2008), Summer Asian-Pacific oscillation and its relationship with atmospheric circulation and monsoon rainfall, Acta Meteorol. Sin., 22, 455471.
  • Zhao, P., Z. H. Cao, and J. M. Chen (2009), A summer teleconnection over the extratropical Northern Hemisphere and associated mechanisms, Clim. Dyn., doi:10.1007/s00382-009-0699-0.
  • Zhao, P., S. Yang, and R. C. Yu (2010), Long-term changes in rainfall over Eastern China and large-scale atmospheric circulation associated with recent global warming, J. Clim., 23, 15441562.
  • Zhao, Y., P. Braconnot, O. Marti, S. P. Harrison, C. Hewitt, A. Kitoh, Z. Liu, U. Mikolajewicz, B. Otto-Bliesner, and S. L. Weber (2005), A multi-model analysis of the role of the ocean on the African and Indian monsoon during the mid-Holocene, Clim. Dyn., 25, 777800.
  • Zheng, Y. Q., G. Yu, S. M. Wang, B. Xue, D. Q. Zhuo, X. M. Zeng, and H. Q. Liu (2004), Simulation of paleoclimate over East Asia at 6 ka BP and 21 ka BP by a regional climate model, Clim. Dyn., 23, 513529.
  • Zhou, B. T., and P. Zhao (2009), Analysis of the coupled simulation result of the seasonal evolution of the southwesterly wind climate over eastern China in the mid-Holocene, Quat. Sci., 29, 211220.
  • Zhou, T. J., and J. Zhang (2009), Harmonious inter-decadal changes of July–August upper tropospheric temperature across the North Atlantic, Eurasian continent and North Pacific, Adv. Atmos. Sci., 26, 656665.