Acta Geographica Sinica ›› 2015, Vol. 70 ›› Issue (3): 355-363.doi: 10.11821/dlxb201503001
• Orginal Article • Next Articles
Quansheng GE, Jingyun ZHENG, Zhixin HAO()
Received:
2014-12-19
Revised:
2015-02-06
Online:
2015-03-20
Published:
2015-03-20
Quansheng GE, Jingyun ZHENG, Zhixin HAO. PAGES synthesis study on climate changes in Asia over the last 2000 years: Progresses and perspectives[J].Acta Geographica Sinica, 2015, 70(3): 355-363.
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Fig. 2
Synthetic reconstructions of temperature change for the past 1200 years over Asia a. Summer temperature for Asia at a 30-year time resolution; referenced period: 1851-1950; b. Summer temperature for East Asia at an annual time resolution, referenced period: 1961-1990; c. Annual temperature of China at a 10-year time resolution, referenced period: 1851-1950.
[1] | PAGES. Science Plan and Implementation Strategy (IGBP Report No.57). Stockholm: IGBP Secretariat, 2009: 67. |
[2] | Alverson K, Bradley R S, Pedersen T F.Paleoclimate, Global Change and the Future. Berlin: Springer Verlag, 2003: 220. |
[3] | Jones P D, Mann M E.Climate over past millennia. Reviews of Geophysics, 2004, 42(2): 1-42. |
[4] | Jones P, Briffa K, Osborn T et al. High-resolution palaeoclimatology of the last millennium: A review of current status and future prospects. The Holocene, 2009, 19(1): 3-49. |
[5] | Mann M E, Bradley R S, Hughes M K.Northern hemisphere temperatures during the past millennium: Inferences, uncertainties, and limitations. Geophysical Research Letters, 1999, 26: 759-762. |
[6] | Esper J, Cook E R, Schweingruber F H.Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability. Science, 2002, 295: 2250-2253. |
[7] | Cook E R, Esper J, D'Arrigo R. Extra-tropical Northern Hemisphere land temperature variability over the past 1000 years. Quaternary Science Reviews, 2004, 23(20-22): 2063-2074. |
[8] | 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: 613-617. |
[9] | Hegerl G C, Crowley T J, Hyde W T et al. Climate sensitivity constrained by temperature reconstructions over the past seven centuries. Nature, 2006, 440: 1029-1032. |
[10] | D’Arrigo R, Wilson R, Jacoby G. On the long-term context for late twentieth century warming. Journal of Geophysical Research: Atmospheres, 2006, 111: D03103. doi: 10.1029/2005JD006352. |
[11] | Osborn T J, Briffa K R.The spatial extent of 20th-century warmth in the context of the past 1200 years. Science, 2006, 311: 841-844. |
[12] | Loehle C.A 2000-year global temperature reconstruction based on non-tree ring proxies. Energy & Environment, 2007, 18: 1049-1058. |
[13] | Mann M E, Zhange Z H, Hughes M K et al. Proxy-based reconstructions of hemispheric and global surface temperature variations over the past two millennia. Proceedings of the National Academy of Sciences of the United States of America, 2008, 105: 13252-13257. |
[14] | Mann M E, Zhange Z H,Rutherford S et al. Global signatures and dynamical origins of the Little Ice Age and medieval climate anomaly. Science, 2009, 326(5957): 1256-1260. |
[15] | Ljungqvist F C, Fredrik C.A New Reconstruction of temperature variability in the extra-tropical Northern Hemisphere during the Last Two Millennia. Geografiska Annaler Series A: Physical Geography, 2010, 92(3): 339-351. |
[16] | Mcshane B B, Wyner A J.A statistical analysis of multiple temperature proxies: Are reconstructions of surface temperatures over the last 1000 years reliable. Annals of Applied Statistics, 2011, 5(1): 5-44. |
[17] | Christiansen B, Ljungqvist F C.The extra-tropical Northern Hemisphere temperature in the last two millennia: Reconstructions of low-frequency variability. Climate of the Past, 2012, 8(2): 765-786. |
[18] | PAGES 2k Consortium. Continental-scale temperature variability during the past two millennia. Nature Geoscience, 2013, 6: 339-346. |
[19] | IPCC. Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge, United Kingdom and New York, NY, USA: Cambridge University Press, 2001: 101-181. |
[20] | IPCC. Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change., Cambridge, United Kingdom and New York, NY, USA: Cambridge University Press, 2007: 466-482. |
[21] | IPCC. Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge, United Kingdom and New York, NY, USA Cambridge University Press, 2013: 383-464. |
[22] | PAGES. Science Plan and Implementation Strategy (IGBP Report No.57). Stockholm: IGBP Secretariat, 2009: 67. |
[23] | Kaufman D S.PAGES2k Consortium. A community-driven framework for climate reconstructions. Transactions American Geophysical Union, 2014, 95(40): 361-362. |
[24] | Anchukaitis K J, Mckay N.PAGES2k: Advances in climate field reconstructions. Pages Magazine, 2014, 22(2): 7. |
[25] | Takeshi N, Masaki S.Report on the First Asia2k Regional Workshop. PAGES News, 2011, 19(1): 38. |
[26] | Masaki S, Shi F, Takeshi N et al. 2nd Workshop of the PAGES Asia2k Working Group. PAGES News, 2012, 20(2): 93. |
[27] | Ge Q S, Hao Z X, Shao X M et al. Understanding and reconstructing the Asian climate of the last 2000 years. Pages Magazine, 2014, 22(2): 8. |
[28] | Cook E R, Krusic P J,Anchukaitis K J et al. Tree-ring reconstructed summer temperature anomalies for temperate East Asia since 800 C.E. Climate Dynamics, 2013, 41: 2957-2972. |
[29] | Ge Q S, Hao Z X,Zheng J Y et al. Temperature changes over the past 2000 yr in China and comparison with the Northern Hemisphere. Climate of the Past, 2013, 9(3): 1153-1160. |
[30] | Cook E R, Anchukaitis K J, Buckley B M et al. Asian monsoon failure and megadrought during the last millennium. Science, 2010, 328: 486-489. |
[31] | Ummenhofer C C, D'Arrigo R D, Anchukaitis K J et al. Links between Indo-Pacific climate variability and drought in the Monsoon Asia Drought Atlas. Climate Dynamics, 2013, 40: 1319-1334. |
[32] | Yang F M, Shi F, Kang S Y et al. Comparison of the dryness/wetness index in China with the Monsoon Asia Drought Atlas. Theoretical and Applied Climatology, 2013, 114(3/4): 553-566. |
[33] | Ge Quansheng, Zheng Jingyun, Hao Zhixin et al. State-of-the-arts in the study of climate changes over China for the past 2000 years. Acta Geographica Sinica, 2014, 69(9): 1248-1258. |
[葛全胜, 郑景云, 郝志新等. 过去2000年中国气候变化研究的新进展. 地理学报, 2014, 69(9): 1248-1258.] | |
[34] | Nakatsuka T, Tada R, Kawamura K.Editorial: How does research in Japan contribute to the global body of paleoscientific knowledge? PAGES News, 2012, 20(2): 59. |
[35] | Kwak J H, Lee K S, Lim S S et al. Historical responses of Quercus variabilis growth to environmental changes in Southern Korea: Evidence from tree ring width and δ13C. Journal of the Korean Society for Applied Biological Chemistry, 2013, 56(5): 583-590. |
[36] | Wright W E, Guan B T, Tseng Y H et al. Reconstruction of the springtime East Asian Subtropical Jet and Western Pacific pattern from a millennial-length Taiwanese tree-ring chronology. Climate Dynamics, 2014: 1-15. |
[37] | Wiles G C, Solomina O, D'Arrigo R et al. Reconstructed summer temperatures over the last 400 years based on larch ring widths: Sakhalin Island, Russian Far East. Climate Dynamics, 2014: 1-9. |
[38] | Davi N, Jacoby G, Fang K et al. Reconstructing drought variability for Mongolia based on a large-scale tree ring network: 1520-1993. Journal of Geophysical Research-Atmospheres, 2011, 115: D22103. doi: 10.1029/2010JD013907. |
[39] | Zhang T, Yuan Y, He Q et al. Development of tree-ring width chronologies and tree-growth response to climate in the mountains surrounding the Issyk-Kul Lake, Central Asia. Dendrochronologia, 2014, 32(3): 230-236. |
[40] | Bräuning A.Dendroecology in Asia. Trees, 2013, 27(2): 341-342. |
[41] | Borgaonkar H P, Sikder A B, Ram S.High altitude forest sensitivity to the recent warming: A tree-ring analysis of conifers from Western Himalaya, India. Quaternary International, 2011, 236(1): 158-166. |
[42] | Buckley B M, Anchukaitis K J,Penny D et al. Climate as a contributing factor in the demise of Angkor, Cambodia. Proceedings of the National Academy of Sciences, 2010, 107(15): 6748-6752. |
[43] | Pumijumnong N, Eckstein D.Reconstruction of pre-monsoon weather conditions in northwestern Thailand from the tree-ring widths of Pinus merkusii and Pinus kesiya. Trees, 2011, 25(1): 125-132. |
[44] | Pumijumnong N.Dendrochronology in Southeast Asia. Trees, 2013, 27(2): 343-358. |
[45] | Ahmed M, Palmer J, Khan N et al. The dendroclimatic potential of conifers from northern Pakistan. Dendrochronologia, 2011, 29(2): 77-88. |
[46] | Sano M, Ramesh R, Sheshshayee M S et al. Increasing aridity over the past 223 years in the Nepal Himalaya inferred from a tree-ring δ18O chronology. The Holocene, 2011, 22(7): 809-817. |
[47] | Ge Quansheng, Zheng Jingyun.Progress on the study of the forcing and impacts of the warm periods in China during the past 2000 years. Geographical Research, 2012, 31(4): 769. |
[葛全胜, 郑景云. 过去2000年全球典型暖期的形成机制及其影响研究进展. 地理研究, 2012, 31(4): 769.] | |
[48] | Zhang De'er. A Compendium of Chinese Meteorological Records of the Last 3,000 Years. Nanjing: Jiangsu Education Press, 2004: 1-3666. |
[张德二. 中国三千年气象记录总集. 南京: 江苏教育出版社, 2004: 1-3666.] | |
[49] | Zheng Jingyun, Hao Zhixin, Di Xiaochun.A study on the establishment and application environmental change database during historical times. Geographical Research, 2002, 21(2): 146-154. |
[郑景云, 郝志新, 狄小春. 历史环境变化数据库的建设与应用. 地理研究, 2002, 21(2): 146-154.] | |
[50] | Wang S W, Wen X Y, Luo Y et al. Reconstruction of temperature series of China for the last 1000 years. Chinese Science Bulletin, 2007, 52(23): 3272-3280. |
[51] | Ge Q S, Zheng J Y, Fang X Q 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. The Holocene, 2003, 13(6): 933-940. |
[52] | Yao TD, Masson-Delmotte V, Gao J et al. A review of climatic controls on δ18O in precipitation over the Tibetan Plateau: Observations and simulations. Reviews of Geophysics, 2013, 51(4): 525-548. |
[53] | Zheng J Y, Wang W C, Ge Q S et al. Precipitation variability and extreme events in eastern China during the past 1500 years. Terrestrial Atmospheric and Oceanic Sciences, 2006, 17(3): 579-592. |
[54] | Yang B, Qin C, Wang J L et al. A 3,500-year tree-ring record of annual precipitation on the northeastern Tibetan Plateau. Proceedings of the National Academy of Sciences of the United States of America, 2014, 111(8): 2903-2908. |
[55] | 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. Geophysical Research Letters, 2010, 37: L03703. |
[56] | Shao X M, Xu Y, Yin Z Y et al. Climatic implications of a 3585-year tree-ring width chronology from the northeastern Qinghai-Tibetan Plateau. Quaternary Science Reviews, 2010, 29: 2111-2122. |
[57] | Ge Quansheng.The Climate Change in China during the Past Dynasties. Beijing: Science Press, 2011: 61-665. |
[葛全胜. 中国历朝气候变化. 北京: 科学出版社, 2011: 61-665.] | |
[58] | Chu G Q, Sun Q,Wang X H et al. Seasonal temperature variability during the past 1600 years recorded in historical documents and varved lake sediment profiles from northeastern China. The Holocene, 2012, 22(7): 785-792. |
[59] | Hao Z X, Zheng J Y, Ge Q S et al. Winter temperature variations over the middle and lower reaches of the Yangtze River since 1736 AD. Climate of the Past, 2012, 8(3): 1023-1030. |