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A tree-ring based precipitation reconstruction for the Mohe region in the northern Greater Higgnan Mountains, China, since AD 1724

Published online by Cambridge University Press:  20 January 2017

Abstract

August–July precipitation has been reconstructed back to AD 1724 for the Mohe region in the northern Greater Higgnan Mountains, China, using Pinus sylvestris var. mongolica tree-ring width. The reconstruction explains 39% of the variance in the precipitation observed from AD 1960–2008. Some droughts noted in historical documents are precisely captured in our reconstruction. Wet periods occurred during the periods of AD 1734–1785, AD 1805–1830, AD 1863–1880, AD 1922–1961, and AD 1983–1998; while the periods of AD 1786–1804, AD 1831–1862, AD 1881–1921, and AD 1962–1982 were relatively dry. Power spectral and wavelet analyses demonstrated the existence of significant 24-yr, 12-yr, and 2-yr cycles of variability. The results of the spatial correlations suggest that our reconstruction contains climatic signals for the southern Stanovoy Range and the northern Greater Higgnan Mountains. The positive correlations between the new reconstructed precipitation series and two precipitation reconstructions indicate that our precipitation reconstruction captures broad-scale regional climatic variations. A comparison between the weakening tendency of summer monsoon and the dry period of our reconstruction reveals that the annual precipitation in the Mohe region is partly influenced by the East Asian Summer Monsoon.

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Articles
Copyright
University of Washington

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References

Baldwin, M.P., Gray, L.J., Dunkerton, T.J., Hamilton, K., Haynes, P.H., Randel, W.J., Holton, J.R., Alexander, M.J., Hirota, I., Horinouchi, T., Jones, D.B.A., Kinnersley, J.S., Marquardt, C., Sato, K., and Takahashi, M. The quasi-biennial oscillation. Reviews of Geophysics 39, (2001). 179229.Google Scholar
Briffa, K.R., Osborn, T.J., Schweingruber, F.H., Harris, I.C., Jones, P.D., Shiyatov, S.G., and Vaganov, E.A. Low-frequency temperature variations from a northern tree ring density network. Journal of Geophysical Research 106, (2001). 29292941.Google Scholar
Büntgen, U., Tegel, W., Nicolussi, K., McCormick, M., Frank, D., Trouet, V., Kaplan, J.O., Herzig, F., Heussner, K.U., Wanner, H., Luterbacher, J., and Esper, J. 2500 years of European climate variability and human susceptibility. Science 331, (2011). 578582.Google Scholar
Cook, E.R., and Kairiukstis, L.A. Methods of Dendrochronology. (1990). Kluwer Academic Publishers, Dordrecht.Google Scholar
Cook, E.R., and Peters, K. The smoothing spline: a new approach to standardizing forest interior tree-ring width series for dendroclimatic studies. Tree-Ring Bulletin 41, (1981). 4553.Google Scholar
Cook, E.R., Meko, D.M., Stahle, D.W., and Cleaveland, M.K. Drought reconstructions for the continental United States. Journal of Climate 12, (1999). 11451162.Google Scholar
Cook, E.R., Anchukaitis, K.J., Buckley, B.M., D'Arrigo, R.D., Jacoby, G.C., and Wright, W.E. Asian monsoon failure and megadrought during the last millennium. Science 328, (2010). 486489.Google Scholar
Esper, J., Cook, E.R., and Schweingruber, F.H. Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability. Science 295, (2002). 22502253.Google Scholar
FAO, , IIASA, , ISRIC, , ISS-CAS, , JRC, Harmonized World Soil Database (Version 1.2). (2012). FAO, Rome, Italy. (IIASA, Laxenburg, Austia) Google Scholar
Frank, D., and Esper, J. Characterization and climate response patterns of a high-elevation, multi-species tree-ring network in the European Alps. Dendrochronologia 22, (2005). 107121.Google Scholar
Fritts, H.C. Tree Rings and Climate. (1976). Academic Press, London.Google Scholar
Grissino-Mayer, H.D. Evaluating crossdating accuracy: a manual and tutorial for the computer program COFECHA. Tree-Ring Research 57, (2001). 205221.Google Scholar
He, J.C., Wang, L.L., and Shao, X.M. The relationships between Mongolian scotch pine tree ring indices and normalized difference vegetation index in Mohe, China. Quaternary Sciences 25, (2005). 252257. (in Chinese, with English abstract) Google Scholar
Liu, Y., Cai, Q.F., Park, W.K., An, Z.S., and Ma, L.M. Tree-ring precipitation records from Baiyinaobao, Inner Mongolia since A.D. 1838. Chinese Science Bulletin 48, (2003). 11401145.Google Scholar
Liu, Y., Shi, J.F., Shishov, V.V., Vaganov, E.A., Yang, Y.K., Cai, Q.F., Sun, J.Y., Wang, L., and Djanseitov, I. Reconstruction of May–July precipitation in the north Helan Mountain, Inner Mongolia since A.D. 1726 from tree-ring late-wood widths. Chinese Science Bulletin 49, (2004). 405409.Google Scholar
Liu, Y., An, Z.S., Ma, H.Z., Cai, Q.F., Liu, Z.Y., Kutzbach, J.K., Shi, J.F., Song, H.M., Sun, J.Y., Yi, L., and Li, Q. Precipitation variation in the northeastern Tibetan Plateau recorded by the tree rings since 850 AD and its relevance to the Northern Hemisphere temperature. Science in China Series D: Earth Sciences 49, (2006). 408420.Google Scholar
Liu, Y., Bao, G., Song, H.M., Cai, Q.F., and Sun, J.Y. Precipitation reconstruction from Hailar pine (Pinus sylvestris var. mongolica) tree rings in the Hailar region, Inner Mongolia, China back to 1865 AD. Palaeogeography, Palaeoclimatology, Palaeoecology 282, (2009). 8187.Google Scholar
Liu, Y., Tian, H., Song, H.M., and Liang, J.M. Tree ring precipitation reconstruction in the Chifeng–Weichang region, China, and East Asian summer monsoon variation since A.D. 1777. Journal of Geophysical Research 115, (2010). D06103 http://dx.doi.org/10.1029/2009JD012330 Google Scholar
Liu, Y., Wang, C.Y., Hao, W.J., Song, H.M., Cai, Q.F., Tian, H., Sun, B., and Linderholm, H.W. Tree-ring-based annual precipitation reconstruction in Kalaqin, Inner Mongolia for the last 238 years. Chinese Science Bulletin 56, (2011). 29953002.Google Scholar
Michaelsen, J. Cross-validation in statistical climate forecast models. Journal of Climate and Applied Meteorology 26, (1987). 15891600.Google Scholar
Mitchell, T.D., and Jones, P.D. An improved method of constructing a database of monthly climate observations and associated high-resolution grids. International Journal of Climatology 25, (2005). 693712.CrossRefGoogle Scholar
Nagovitsyn, Y.A. A nonlinear mathematical model for the solar cyclicity and prospects for reconstructing the solar activity in the past. Astronomy Letters 23, (1997). 742748.Google Scholar
NMIC China Monthly Surface Climatological Database. (2008). NMIC, Beijin, China.Google Scholar
Palmer, J., Lorrey, A., Turney, C.S.M., Hogg, A., Baillie, M., Fifield, K., and Ogden, J. Extension of New Zealand kauri (Agathis australis) tree-ring chronologies into Oxygen Isotope Stage (OIS) 3. Journal of Quaternary Science 21, (2006). 779787.Google Scholar
Pederson, N., Jacoby, G.C., D'arrigo, R.D., Cook, E.R., Buckley, B.M., Dugarjav, C., and Mijiddorj, R. Hydrometeorological reconstructions for northeastern Mongolia derived from tree rings: 1651–1995. Journal of Climate 14, (2001). 872881.Google Scholar
Stokes, M.A., and Smiley, T.L. An Introduction to Tree-ring Dating. (1996). University of Arizona Press, Tucson. (Originally published: 1968 by the University of Chicago Press, Chicago) Google Scholar
Sun, Y., Wang, L.L., Chen, J., and Duan, J.P. Reconstructing mean maximum temperatures of May–August from tree-ring maximum density in North Da Hinggan Mountains, China. Chinese Science Bulletin 57, (2012). 20072014.Google Scholar
Sun, F.H., Yuan, J., and Lu, S. The change and test of climate in northeast China over the last 100 years. Climatic and Environmental Research 11, (2006). 101108. (in Chinese, with English abstract) Google Scholar
Torrence, C., and Compo, G.P. A practical guide to wavelet analysis. Bulletin of the American Meteorological Society 79, (1998). 6178.2.0.CO;2>CrossRefGoogle Scholar
Wang, Z. Phytophysiology. (2000). China Agriculture Press, Beijing. (in Chinese) Google Scholar
Wang, H.J. The weakening of the Asian monsoon circulation after the end of 1970's. Advances in Atmospheric Sciences 18, (2001). 376386.Google Scholar
Wang, L.L., Shao, X.M., Huang, L., and Liang, E.Y. Tree-ring characteristics of Larix gmelinii and Pinus sylvestris var. mongolica and their response to climate in Mohe, China. Acta Phytoecologica Sinica 29, (2005). 380385. (in Chinese, with English abstract) Google Scholar
Wen, K.G., and Shen, J.G. The Documents of Chinese Meteorological Disaster: Volume of Inner Mongolia Province. (2008). Meteorological Publishers, Beijing. (in Chinese) Google Scholar
Wen, K.G., and Sun, Y.G. The Documents of Chinese Meteorological Disaster: Volume of Heilongjiang Province. (2007). Meteorological Publishers, Beijing. (in Chinese) Google Scholar
Wigley, T.M.L., Briffa, K.R., and Jones, P.D. On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. Journal of Climate and Applied Meteorology 23, (1984). 201203.Google Scholar
Wu, X.P., Zhu, B., Zhao, S.Q., Piao, S.L., and Fang, J.Y. Comparison of community structure and species diversity of mixed forests of deciduous broad-leaved tree and Korean pine in Northeast China. Biodiversity Science 12, (2004). 174181. (in Chinese, with English abstract) Google Scholar
Yu, D.S., and Shi, X.Z. Tentative assessment of soil moisture regime in China. Journal of Natural Resources 13, (1998). 229233. (in Chinese, with English abstract) Google Scholar
Yu, R.C., and Zhou, T.J. Seasonality and three-dimensional structure of the interdecadal change in East Asian monsoon. Journal of Climate 20, (2007). 53445355.Google Scholar