Science China Earth Sciences

, Volume 55, Issue 12, pp 2058–2067 | Cite as

Preliminary multiproxy surface air temperature field reconstruction for China over the past millennium

Research Paper

Abstract

We present the first millennial-length gridded field reconstruction of annual temperature for China, and analyze the reconstruction for spatiotemporal changes and associated uncertainties, based on a network of 415 well-distributed and accurately dated climatic proxy series. The new reconstruction method is a modified form of the point-by-point regression (PPR) approach. The main difference is the incorporation of the “composite plus scale” (CPS) and “Regularized errors-in-variables” (EIV) algorithms to allow for the assimilation of various types of the proxy data. Furthermore, the search radius is restricted to a grid size; this restriction helps effectively exclude proxy data possibly correlated with temperature but belonging to a different climate region. The results indicate that: 1) the past temperature record in China is spatially heterogenic, with variable correlations between cells in time; 2) the late 20th century warming in China probably exceeds mean temperature levels at any period of the past 1000 years, but the temperature anomalies of some grids in eastern China during the Medieval climate anomaly period are warmer than during the modern warming; 3) the climatic variability in the eastern and western regions of China was not synchronous during much of the last millennium, probably due to the influence of the Tibetan Plateau. Our temperature reconstruction may serve as a reference to test simulation results over the past millennium, and help to finely analyze the spatial characteristics and the driving mechanism of the past temperature variability. However, the lower reconstruction skill scores for some grid points underline that the present set of available proxy data series is not yet sufficient to accurately reconstruct the heterogeneous climate of China in all regions, and that there is the need for more highly resolved temperature proxies, particularly in the Tibetan Plateau.

Keywords

climate change global warming paleoclimatology temperature field reconstruction 

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References

  1. 1.
    Crowley T J. Causes of climate change over the past 1000 years. Science, 2000, 289: 270–277CrossRefGoogle Scholar
  2. 2.
    Crowley T J, Lowery T S. How warm was the medieval warm period? Ambio, 2000, 29: 51–54Google Scholar
  3. 3.
    Briffa K R, Osborn T J, Schweingruber F H, et al. Low-frequency temperature variations from a northern tree ring density network. J Geophys Res, 2001, 106: 2929–2941CrossRefGoogle Scholar
  4. 4.
    Esper J, Cook E, Schweingruber F. Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability. Science, 2002, 295: 2250–2253CrossRefGoogle Scholar
  5. 5.
    Moberg A, Sonechkin D M, Holmgren K, et al. Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data. Nature, 2005, 433: 613–617CrossRefGoogle Scholar
  6. 6.
    Mann M E, Zhang Z H, Rutherford S, et al. Global signatures and dynamical origins of the Little Ice Age and Medieval climate anomaly. Science, 2009, 326: 1256–1260CrossRefGoogle Scholar
  7. 7.
    Ljungqvist F C, Krusic P J, Brattström G, et al. Northern Hemisphere temperature patterns in the last 12 centuries. Clim Past 2012, 8: 227–249CrossRefGoogle Scholar
  8. 8.
    Casty C, Raible C C, Stocker T F, et al. A European pattern climatology 1766–2000. Clim Dynam, 2007, 29: 791–805CrossRefGoogle Scholar
  9. 9.
    Guiot J, Nicault A, Rathgeber C, et al. Last-millennium summer-temperature variations in western Europe based on proxy data. Holocene, 2005, 15: 489–500CrossRefGoogle Scholar
  10. 10.
    Luterbacher J, Dietrich D, Xoplaki E, et al. European seasonal and annual temperature variability, trends, and extremes since 1500. Science, 2004, 303: 1499–1503CrossRefGoogle Scholar
  11. 11.
    Pauling A, Luterbacher J, Casty C, et al. Five hundred years of gridded high-resolution precipitation reconstructions over Europe and the connection to large-scale circulation. Clim Dynam, 2006, 26: 387–405CrossRefGoogle Scholar
  12. 12.
    Riedwyl N, Kuttel M, Luterbacher J, et al. Comparison of climate field reconstruction techniques: Application to Europe. Clim Dynam, 2009, 32: 381–395CrossRefGoogle Scholar
  13. 13.
    Cook E, Woodhouse C, Eakin C, et al. Long-term aridity changes in the western United States. Science, 2004, 306: 1015–1018CrossRefGoogle Scholar
  14. 14.
    Neukom R, Luterbacher J, Villalba R, et al. Multi-centennial summer and winter precipitation variability in southern South America. Geophys Res Lett, 2010, 37, doi: 10.1029/2010GL043680Google Scholar
  15. 15.
    Neukom R, Luterbacher J, Villalba R, et al. Multiproxy summer and winter surface air temperature field reconstructions for southern South America covering the past centuries. Clim Dynam, 2011, 37: 35–51CrossRefGoogle Scholar
  16. 16.
    Wang S W, Wen X Y, Luo Y, et al. Reconstruction of temperature series of China for the last 1000 years. Chin Sci Bull, 2007, 52: 3272–3280CrossRefGoogle Scholar
  17. 17.
    Yang B, Braeuning A, Johnson K, et al. General characteristics of temperature variation in China during the last two millennia. Geophys Res Lett, 2002, 29: 38–31Google Scholar
  18. 18.
    Ge Q S, Zheng J Y, Hao Z X, et al. Temperature variation through 2000 years in China: An uncertainty analysis of reconstruction and regional difference. Geophys Res Lett, 2010, 37, doi: 10.1029/2009gl041281Google Scholar
  19. 19.
    Ge Q, Zheng J, Fang X, et al. Winter half-year temperature reconstruction for the middle and lower reaches of the Yellow River and Yangtze River, China, during the past 2000 years. Holocene, 2003, 13: 933–940Google Scholar
  20. 20.
    Liu Y, An Z, Linderholm H, et al. Annual temperatures during the last 2485 years in the mid-eastern Tibetan Plateau inferred from tree rings. Sci China Ser D-Earth Sci, 2009, 52: 348–359CrossRefGoogle Scholar
  21. 21.
    Tan M, Liu T, Hou J, et al. Cyclic rapid warming on centennial-scale revealed by a 2650-year stalagmite record of warm season temperature. Geophys Res Lett, 2003, 30: 1617–1620CrossRefGoogle Scholar
  22. 22.
    Yao T D, Guo X J, Thompson L, et al. δ 18O record and temperature change over the past 100 years in ice cores on the Tibetan Plateau. Sci China Ser D-Earth Sci, 2006, 49: 1–9CrossRefGoogle Scholar
  23. 23.
    Shao X, Wang S, Zhu H, et al. A 3585-year ring-width dating chronology of Qilian juniper from the northeastern Qinghai-Tibetan Plateau. Iawa J, 2009, 30: 379–394Google Scholar
  24. 24.
    Zhang Y, Gou X, Chen F, et al. A 1232-year tree-ring record of climate variability in the Qilian Mountains, northwestern China. Iawa J, 2009, 30: 407–420Google Scholar
  25. 25.
    Liu X, Shao X, Zhao L, et al. Dendroclimatic temperature record derived from tree-ring width and stable carbon isotope chronologies in the Middle Qilian Mountains, China. Arct Antarct Alp Res, 2007, 39: 651–657CrossRefGoogle Scholar
  26. 26.
    Zhang Q B, Cheng G D, Yao T D, et al. A 2,326-year tree-ring record of climate variability on the northeastern Qinghai-Tibetan Plateau. Geophys Res Lett, 2003, 30: 1739–1742CrossRefGoogle Scholar
  27. 27.
    Bradley R S. Paleoclimatology: Reconstructing Climates of the Quaternary. 2rd ed. London: Academic Press, 1999Google Scholar
  28. 28.
    Cook E R, Meko D M, Stahle D W, et al. Drought reconstructions for the continental United States. J Clim, 1999, 12: 1145–1162CrossRefGoogle Scholar
  29. 29.
    Cook E R, Anchukaitis K J, Buckley B M, et al. Asian monsoon failure and megadrought during the last millennium. Science, 2010, 328: 486–489CrossRefGoogle Scholar
  30. 30.
    Zheng J, Yin Y, Li B. A new scheme for climate regionalization in China (in Chinese). Acta Geogr Sin, 2010, 65: 3–12Google Scholar
  31. 31.
    Brohan P, Kennedy J, Harris I, et al. Uncertainty estimates in regional and global observed temperature changes: A new dataset from 1850. J Geophys Res, 2006, 111, doi: 10.1029/2005JD006548Google Scholar
  32. 32.
    Li Q X, Dong W J, Li W, et al. Assessment of the uncertainties in temperature change in China during the last century. Chin Sci Bull, 2010, 55: 1974–1982CrossRefGoogle Scholar
  33. 33.
    Fang K Y, Gou X H, Chen F H, et al. Large-Scale Precipitation Variability over Northwest China Inferred from Tree Rings. J Clim, 2011, 24: 3457–3468CrossRefGoogle Scholar
  34. 34.
    Zhu H, Zheng Y, Shao X, et al. Millennial temperature reconstruction based on tree-ring widths of Qilian juniper from Wulan, Qinghai Province, China. Chin Sci Bull, 2008, 53: 3914–3920CrossRefGoogle Scholar
  35. 35.
    Liu Y, An Z, Ma H, et al. Precipitation variation in the northeastern Tibetan Plateau recorded by the tree rings since 850 AD and its relevance to the Northern Hemisphere temperature. Sci China Ser D-Earth Sci, 2006, 49: 408–420CrossRefGoogle Scholar
  36. 36.
    Briffa K R, Melvin T M. A closer look at regional curve standardization of tree-ring records: Justification of the need, a warning of some pitfalls, and suggested improvements in its application. In: Hughes M K, Swetnam T W, Diaz H F, eds. Dendroclimatology: Progress and Prospects. Heidelberg: Springer, 2011. 113–145Google Scholar
  37. 37.
    Yang B. Spatial and temporal patterns of climate variations over the Tibetan Plateau during the period 1300–2010 (in Chinese). Quat Sci, 2012, 32: 81–94Google Scholar
  38. 38.
    Yi L, Yu H, Ge J, et al. Reconstructions of annual summer precipitation and temperature in north-central China since 1470 AD based on drought/flood index and tree-ring records. Clim Change, 2011, 110: 469–498CrossRefGoogle Scholar
  39. 39.
    Li Z S, Zhang Q B, Ma K. Tree-ring reconstruction of summer temperature for AD 1475–2003 in the central Hengduan Mountains, Northwestern Yunnan, China. Clim Change, 2011, 110: 455–467CrossRefGoogle Scholar
  40. 40.
    Christiansen B, Ljungqvist F C. Reconstruction of the extratropical NH mean temperature over the last millennium with a method that preserves low-frequency variability. J Clim, 2011, 24: 6013–6034CrossRefGoogle Scholar
  41. 41.
    Yang B, Qin C, Huang K, et al. Spatial and temporal patterns of variations in tree growth over the northeastern Tibetan Plateau during the period AD 1450–2001. Holocene, 2010, 20: 1235–1245CrossRefGoogle Scholar
  42. 42.
    Yang B, Kang X C, Liu J J, et al. Annual temperature history in Southwest Tibet during the last 400 years recorded by tree rings. Int J Climatol, 2010, 30: 962–971Google Scholar
  43. 43.
    Yang B, Kang X C, Brauning A, et al. A 622-year regional temperature history of southeast Tibet derived from tree rings. Holocene, 2010, 20: 181–190CrossRefGoogle Scholar
  44. 44.
    Fan Z, Brauning A, Tian Q, et al. Tree ring recorded May–August temperature variations since AD 1585 in the Gaoligong Mountains, southeastern Tibetan Plateau. Palaeogeogr Palaeoclimatol Palaeoecol, 2010, 296: 94–102CrossRefGoogle Scholar
  45. 45.
    Tan L, Cai Y, Cheng H, et al. Summer monsoon precipitation variations in central China over the past 750 years derived from a high-resolution absolute-dated stalagmite. Palaeogeogr Palaeoclimatol Palaeoecol, 2009, 280: 432–439CrossRefGoogle Scholar
  46. 46.
    Liang E, Shao X, Xu Y. Tree-ring evidence of recent abnormal warming on the southeast Tibetan Plateau. Theor Appl Climatol, 2009, 98: 9–18CrossRefGoogle Scholar
  47. 47.
    Fan Z X, Brauning A, Yang B, et al. Tree ring density-based summer temperature reconstruction for the central Hengduan Mountains in southern China. Global Planet Change, 2009, 65: 1–11CrossRefGoogle Scholar
  48. 48.
    Zhang P, Cheng H, Edwards R, et al. A test of climate, Sun, and culture relationships from an 1810-year Chinese cave record. Science, 2008, 322: 940–942CrossRefGoogle Scholar
  49. 49.
    Mann M E, Zhang Z H, Hughes M K, et al. Proxy-based reconstructions of hemispheric and global surface temperature variations over the past two millennia. Proc Natl Acad Sci USA, 2008, 105: 13252–13257CrossRefGoogle Scholar
  50. 50.
    Liang E, Shao X, Qin N. Tree-ring based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau. Global Planet Change, 2008, 61: 313–320CrossRefGoogle Scholar
  51. 51.
    Hu C, Henderson G M, Huang J, et al. Quantification of Holocene Asian monsoon rainfall from spatially separated cave records. Earth Planet Sc Lett, 2008, 266: 221–232CrossRefGoogle Scholar
  52. 52.
    Fan Z, Brauning A, Cao K. Annual temperature reconstruction in the Central Hengduan Mountains, China, as deduced from tree rings (in Chinese). Dendrochronologia, 2008, 26: 97–107CrossRefGoogle Scholar
  53. 53.
    Gou X H, Chen F H, Jacoby G, et al. Rapid tree growth with respect to the last 400 years in response to climate warming, northeastern Tibetan Plateau. Int J Climatol, 2007, 27: 1497–1503CrossRefGoogle Scholar
  54. 54.
    Thompson L G, Yao T, Davis M E, et al. Holocene climate variability archived in the Puruogangri ice cap on the central Tibetan Plateau. Ann Glaciol, 2006, 43: 61–69CrossRefGoogle Scholar
  55. 55.
    Thompson L G, Mosley-Thompson E, Brecher H, et al. Abrupt tropical climate change: Past and present. Proc Natl Acad Sci USA, 2006, 103: 10536–10543CrossRefGoogle Scholar
  56. 56.
    Thompson L, Mosley-Thompson E, Davis M, et al. Tropical glacier and ice core evidence of climate change on annual to millennial time scales. Clim Change, 2003, 59: 137–155CrossRefGoogle Scholar
  57. 57.
    Cook E R, Krusic P J, Jones P D. Dendroclimatic signals in long tree-ring chronologies from the Himalayas of Nepal. Int J Climatol, 2003, 23: 707–732CrossRefGoogle Scholar
  58. 58.
    Esper J, Schweingruber F, Winiger M. 1300 years of climatic history for Western Central Asia inferred from tree-rings. Holocene, 2002, 12: 267–277CrossRefGoogle Scholar
  59. 59.
    D’Arrigo R, Jacoby G, Frank D, et al. 1738 years of Mongolian temperature variability inferred from a tree-ring width chronology of Siberian pine. Geophys Res Lett, 2001, 28: 543–546CrossRefGoogle Scholar
  60. 60.
    Thompson L, Yao T, Mosley-Thompson E, et al. A high-resolution millennial record of the South Asian monsoon from Himalayan ice cores. Science, 2000, 289: 1916CrossRefGoogle Scholar
  61. 61.
    Li J, Yuan Y, You X. The Tree-ring Hydrology Research and Application (in Chinese). Beijing: Science Press, 2000Google Scholar
  62. 62.
    Liu H B, Shao X M. Reconstruction of earlyspring temperature at Zhenan from 1755 using tree ring chronology (in Chinese). Acta Meteorol Sin, 2000, 58: 223–234Google Scholar
  63. 63.
    Shao X, Fan J. Past climate on west Sichuan Plateau as reconstructed from ring-widths of dragon spruce (in Chinese). Quat Sci, 1999, 1: 81–89Google Scholar
  64. 64.
    Ku T L, Li H C. Speleothems as high-resolution paleoenvironment archives: Records from northeastern China. P Indian Earth, 1998, 107: 321–330Google Scholar
  65. 65.
    Kitagawa H, Matsumoto E. Climatic implications of δ 13C variations in a Japanese cedar (Cryptomeria japonica) during the last two millenia. Geophys Res Lett, 1995, 22: 2155–2158CrossRefGoogle Scholar
  66. 66.
    Wang W C, Portman D, Gong G, et al. Beijing summer temperatures since 1724. In: Bradley R S, Jones P D, eds. Climate since A. D. 1500. London and New York: Routledge, 1992. 679Google Scholar
  67. 67.
    Wang R, Wang S, Fraedrich K. An approach to reconstruction of temperature on a seasonal basis using historical documents from China. Int J Climatol, 1991, 11: 381–392CrossRefGoogle Scholar
  68. 68.
    Wang S, Wang R. Seasonal and annual temperature variations since 1470 AD in East China (in Chinese). Acta Meteorol Sin, 1990, 4: 428–439Google Scholar
  69. 69.
    Zhang D. Winter temperature changes during the last 500 years in South China. Chin Sci Bull, 1980, 25: 497–500Google Scholar
  70. 70.
    Zhang Q, Gemmer M, Chen J. Climate changes and flood/drought risk in the Yangtze Delta, China, during the past millennium. Quatern Int, 2008, 176–177: 62–69CrossRefGoogle Scholar
  71. 71.
    Bräuning A, Grießinger J. Late Holocene variations in monsoon intensity in the Tibetan-Himalayan region—Evidence from tree rings. J Geol Soc India, 2006, 68: 485–493Google Scholar
  72. 72.
    Wang Y, Cheng H, Edwards R L, et al. The Holocene Asian Monsoon: Links to solar changes and north atlantic climate. Science, 2005, 308: 854–857CrossRefGoogle Scholar
  73. 73.
    Qian W, Hu Q, Zhu Y, et al. Centennial-scale dry-wet variations in East Asia. Clim Dynam, 2003, 21: 77–89CrossRefGoogle Scholar
  74. 74.
    Zhang P, Gong G. Some characteristics of climatic fluctuations in China since the 16th century. Acta Meteorol Sin, 1979, 34: 238–247Google Scholar
  75. 75.
    Cook E R, Seager R, Cane M A, et al. North American drought: Reconstructions, causes, and consequences. Earth-Sci Rev, 2007, 81: 93–134CrossRefGoogle Scholar
  76. 76.
    Schneider T. Analysis of incomplete climate data: Estimation of mean values and covariance matrices and imputation of missing values. J Clim, 2001, 14: 853–871CrossRefGoogle Scholar
  77. 77.
    Jones P D, Briffa K R, Osborn T J, et al. High-resolution palaeoclimatology of the last millennium: A review of current status and future prospects. Holocene, 2009, 19: 3–49CrossRefGoogle Scholar
  78. 78.
    Mann M E, Rutherford S, Wahl E, et al. Robustness of proxy-based climate field reconstruction methods. J Geophys Res, 2007, 112, doi: 10.1029/2006jd008272Google Scholar
  79. 79.
    Riedwyl N, Luterbacher J, Wanner H. An ensemble of European summer and winter temperature reconstructions back to 1500. Geophys Res Lett, 2008, 35, doi: 10.1029/2008gl035395Google Scholar
  80. 80.
    Rutherford S, Mann M E, Osborn T J, et al. Proxy-based Northern Hemisphere surface temperature reconstructions: Sensitivity to method, predictor network, target season, and target domain. J Clim, 2005, 18: 2308–2329CrossRefGoogle Scholar
  81. 81.
    McShane B B, Wyner A J. A statistical analysis of multiple temperature proxies: Are reconstructions of surface temperatures over the last 1000 years reliable? Ann Appl Stat, 2011, 5: 5–44CrossRefGoogle Scholar
  82. 82.
    Lee T C K, Zwiers F W, Tsao M. Evaluation of proxy-based millennial reconstruction methods. Clim Dynam, 2008, 31: 263–281CrossRefGoogle Scholar
  83. 83.
    Jones P D, Briffa K R, Barnett T P, et al. High-resolution palaeoclimatic records for the last millennium: Interpretation, integration and comparison with General Circulation Model control-run temperatures. Holocene, 1998, 8: 455–471CrossRefGoogle Scholar

Copyright information

© Science China Press and Springer-Verlag Berlin Heidelberg 2012

Authors and Affiliations

  1. 1.Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research InstituteChinese Academy of SciencesLanzhouChina
  2. 2.State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric PhysicsChinese Academy of SciencesBeijingChina
  3. 3.Oeschger Centre for Climate Change Research & Institute of GeographyUniversity of BernBernSwitzerland

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