THE 1920S DROUGHT RECORDED BY TREE RINGS AND ...

430 ERYUAN LIANG ET AL.Li, W. H., Cheng, X., Liu, Y. D. and Xia, M. F.: 1994 The Top Ten Natural Disasters in ModernChinese History (1840-1949), Shanghai People’s Press, Shanghai, p. 350. (in Chinese)Liang, E. Y., Shao, X. M., Hu, Y. X. and Lin, J. X.: 2001, ‘Dendroclimatic evaluation of climategrowthrelationships of meyer spruce (Picea meyeri) on a sandy substrate in semi-arid grassland,North China’, Trees 15, 230–235.Liang, E. Y., Shao, X. M., Kong, Z. C. and Lin, J. X.: 2003, ‘The extreme drought in the 1920s andits effect on tree growth deduced from tree ring analysis: A case study in north China’, Ann. For.Sci. 60, 145–152.Liu, H. B. and Wu, X. D.: 1996, ‘Spatio-temporal characteristics of the low-flow period from 1922to 1932 in the middle reaches of the yellow river’, Shaanxi Meteorol. 6, 12–15. (in Chinese)Liu, H. B., Shao, X. M., and Huang, L.: 2002, ‘Reconstruction of early-summer drought indices inmid-north region of China after 1500 using tree ring chronologies’, Quat. Sci. 22.Liu, Y. and Ma, L. M.: 1999, ‘Tree-ring seasonal precipitation reconstruction for Mt. Da Qing area,inner Mongolia, China for the last 376 years’, Chin. Sci. Bull. 44, 1986–1992 (in Chinese).Liu, Y., Cai, Q. F., Ma, L. M. and An, Z. S.: 2001, ‘Tree ring precipitation records from Baotou andthe east Asian summer monsoon variation for the last 254 years’, Earth Sci. Frontiers 8, 91–97(in Chinese).Liu, Y., Shao, X. M., Wu, X. D. and Liu, H. B.: 1997, ‘Seasonal temperature and rainfall reconstructionin north-central China from tree-ring density and stable carbon isotope for the last 100 years’,Sci. in China (D) 27, 271–277. (in Chinese)Liu, Y., Shi, J. F., Shishov, V., Vaganov, E., Yang., Y. K., Cai, Q. F., Sun, J. Y., Wang, L. and Djanseitov,I.: 2004, ‘Reconstruction of May–July precipitation in the north Helan mountain, inner mongoliasince A.D. 1726 from tree-ring late-wood widths’, Chin. Sci. Bull. 49, 405–409.Mallory, W.: 1926, China: Land of Famine, American Geographical Society, New York, p.199.Meko, D. M., Stockton, C. W. and Boggess, W. R.: 1995, ‘The tree-ring record of severe sustaineddrought’, Water Resour. Bull. 31, 789–801.Mijiddor, R. and Namhay, A.: 1983, ‘On drought and unfavorable winter conditions recurrence inMongolia’, Transactions of the HMRI, Ulaanbaatar 11, 118–131. (in Russian)Neumann , J. and Dettwiller, J.: 1990, ‘Great historical events that were significantly affected by theweather: Part 9, the year leading to the revolution of 1789 in France (II)’, Bull. Amer. Meteorol.Soc. 71, 33–41.Park, W. K., Kim, Y. J., Lee, J. H. and Seo, J. W.: 2001a, ‘Development of tree-ring chronologies ofPinus densiflora from Mt. Sorak and Dating the years of construction of the Kyunghoe-ru Pavilionin Seoul’, J. Korean Physical Soc. 39, 790–795.Park, W. K., Seo, J. W., Liu, Y., Kim, Y. J. and Han, S. W.: 2001b, ‘Reconstruction of April–Augustprecipitation in Mt. Sorak region from tree rings’, Korea J. Quat. Res. 15, 47–52.Pederson, N., Jacoby, G. C., D’Arrigo, R. D., Cook, E. R., Buckley, B. M., Dugarjav, C. and Mijiddorj,R.: 2001, ‘Hydrometeorological reconstructions for northeastern Mongolia derived from treerings: 1651–1995’, J. Clim. 14, 872–881.Qin, N. S., Jin, L. Y., Shi, X. H., Wang, Q. C., Li, L., Chen, F. and Li, L. M.: 2004, ‘A 518-year runoffreconstruction of Tongtian river basin using tree-ring width chronologies in the source region ofYangtze river’, Acta Geog. Sin. 59, 550–556. (in Chinese with English abstract)Qin, N. S., Shao, X. M., Jin, L. Y., Wang, Q. C., Zhu, X. D., Wang, Z. Y. and Li, J. B.: 2003, ‘Climatechange over southern Qinghai Plateau in the past 500 years recorded in Sabina tibetica tree rings’,Chin. Sci. Bull. 48, 2483–2487.Qian, W. H. and Zhu, Y. F.: 2001, ‘Climate change in China from 1880 to 1998 and Its impact on theenvironmental condition’, Clim. Change 50, 419–444.Qian, W. H., Hu, Q., Zhu, Y. F. and Lee, D. -K.: 2003, ‘Centennial-scale dry-wet variations in eastAsia’, Clim. Dynamics 21, 77–89.