Skip to main content
Log in

A 258-year reconstruction of precipitation for southern Northeast China and the northern Korean peninsula

  • Published:
Climatic Change Aims and scope Submit manuscript

Abstract

We present a well-verified precipitation reconstruction (r = 0.612, p < 0.01), spanning 1741 to 1998, for a relatively humid monsoon region from southern Northeast China and the northern Korean peninsula, based on tree rings from Chinese pine and Korean pine. We then investigate the variability of the reconstruction, and identify the leading rainfall patterns and regional dryness and wetness modes during the latest 2.5 centuries. This reconstruction shows that three persistent dry decades occurred during the 1840s, 1910s and 1850s and the three wettest decades occurred during the 1770s, 1820s and 1930s. The five years with lowest rainfall were 1759, 1917, 1841, 1747 and 1839, and 1770, 1938, 1819, 1941 and 1822 were the five years with highest rainfall, respectively. As indicated by the spatial correlation patterns, the reconstruction also exhibits regional characteristics. The variation of reconstructed rainfall significantly corresponds to East Asian monsoon.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5

Similar content being viewed by others

References

  • Buckley BM, Anchukaitis KJ, Penny D, Fletcher R, Cook ER, Sano M, Nam L, Wichienkeeo A, Minh TT, Hong TM (2010) Climate as a contributing factor in the demise of Angkor, Cambodia. PNAS 107:6748–6752. doi:10.1073/pnas.0910827107

    Article  Google Scholar 

  • Chen Z, He X, Cook ER, He H-S, Chen W, Sun Y, Cui M (2011) Detecting dryness and wetness signals from tree rings in Shenyang, Northeast China. Palaeogeogr Palaeoclimatol Palaeoecol 302:301–310. doi:10.1016/j.palaeo.2011.01.018

    Article  Google Scholar 

  • Cook ER, Woodhouse C, Eakin CM, Meko DM, Stahle DW (2004) Long-Term Aridity Changes in the Western United States. Science 306(5698):1015--1018

  • Cook ER, Anchukaitis KJ, Buckley BM, D’Arrigo RD, Jacoby GC, Wright WE (2010) Asian monsoon failure and megadrought during the last millennium. Science 328:486–489. doi:10.1126/science.1185188

    Article  Google Scholar 

  • Davi NK, Jacoby GC, Curtis AE, Baatarbileg N (2006) Extension of drought records for Central Asia using tree rings: west-Central Mongolia. J Clim 19:288–299

    Article  Google Scholar 

  • Ding Y, Chan JCL (2005) The east Asian summer monsoon: an overview. Meteorog Atmos Phys 89:117–142. doi:10.1007/s00703-005-0125-z

    Article  Google Scholar 

  • Editorial Committee of Academy of Meteorological Science, China Central Meteorological Administration (1981) Yearly charts of dryness/wetness in China for the last 500-year period (in Chinese). Map Publishers, Beijing

    Google Scholar 

  • Fu CB, Fletcher J (1988) Large signal of climatic variation over the ocean in the Asian monsoon region. Adv Atmos Sci 5:389–404

    Article  Google Scholar 

  • Gao Z, Hu Z-Z, Zhu J, Yang S, Zhang R-H, Xiao Z, Jha B (2014) Variability of summer rainfall in Northeast China and its connection with spring rainfall variability in the Huang-Huai region and Indian Ocean SST. J Clim 27:7086–7101. doi:10.1175/JCLI-D-14-00217.1

    Article  Google Scholar 

  • Jung H-S, Lim G-H, Oh J-H (2001) Interpretation of the transient variations in the time series of precipitation amountsin Seoul, Korea. Part I: diurnal variation. J Clim 14:2989–3004

    Article  Google Scholar 

  • Li J, Cook ER, Chen F, Davi N, D’Arrigo R, Gou X, Wright WE, Fang K, Jin L, Shi J, Yang T (2009) Summer monsoon moisture variability over China and Mongolia during the past four centuries. Geophys Res Lett 36:L22705. doi:10.1029/2009GL041162

    Article  Google Scholar 

  • Li J, Zeng Q (2002) A unified monsoon index. Geophys Res Lett 29(8):1274. doi:10.1029/2001GL013874

  • Li J, Zeng Q (2003) A new monsoon index and the geographical distribution of the global monsoons. Adv Atmos Sci 20:299–302

  • Liang EY, Shao XM, Liu HY, Eckstein D (2007) Tree-ring based PDSI reconstruction since AD 1842 in the Ortindag sand land, East Inner Mongolia. Chin Sci Bull 52(19):2715–2721

    Article  Google Scholar 

  • Liu Y, Park W-K, Cai Q, Seo J-W, Sook J-H (2003) Monsoonal precipitation variation in the East Asia since A.D. 1840--Tree-ring evidences from China and Korea. Sci China Ser D 46:1031–1039

    Google Scholar 

  • Liu Y, Tian H, Song H, Liang J (2010) Tree ring precipitation reconstruction in the Chifeng-Weichang region, China, and east Asian summer monsoon variation since a.D. 1777. J Geophys Res 115:1–9. doi:10.1029/2009JD012330

    Google Scholar 

  • Meko DM, Graybill DA (1995) Tree-ring reconstruction of upper Gila River discharge. Water Resour Bull 31:605–616

    Article  Google Scholar 

  • Melvin TM, Briffa KR (2008) A “signal-free” approach to dendroclimatic standardisation. Dendrochronologia 26:71–86

    Article  Google Scholar 

  • Ohyama M, Yonenobu H, Choi J-N, Park W-K, Hanzawa M, Suzuki M (2013) Reconstruction of Northeast Asia spring temperature 1784–1990. Clim Past 9:261–266

    Article  Google Scholar 

  • Park W-K, Seo J-W, Kim Y, Oh J-H (2001) July–August temperature of central Korea since 1700 AD: reconstruction from tree-rings of Korean pine (Pinus koraiensis). Palaeobotanist 50:107–111

    Google Scholar 

  • Pederson N, Jacoby GC, D’Arrigo R, Cook ER, Buckley BM, Dugarjav C, Mijiddorj R (2001) Hydrometeorological reconstructions for northeastern Mongolia derived from tree rings: AD 1651-1995. J Clim 14:872–881

    Article  Google Scholar 

  • Ryan WBF, Carbotte SM, Coplan JO, O’Hara S, Melkonian A, Arko R, Weissel RA, Ferrini V, Goodwillie A, Nitsche F, Bonczkowski J, Zemsky R (2009) Global multi-resolution topography synthesis. Geochem Geophys Geosyst 10:Q03014. doi:10.1029/2008GC002332

    Article  Google Scholar 

  • Shao XM, Wu XD (1997) Reconstruction of climate change on Changbai Mountain, Northeast China using tree-ring data (in Chinese). Quaternary Sci 1:76–85

  • Shen C, Wang W-C, Hao Z, Gong W (2007) Exceptional drought events over eastern China during the last five centuries. Clim Chang 85:453–471

    Article  Google Scholar 

  • Shi JF, Liu Y, Vaganov EA, Li JB, Cai QF (2008) Statistical and process-based modeling analyses of tree growth response to climate in semi-arid area of north Central China: a case study of Pinus tabulaeformis. J Geophys Res 113:G01026. doi:10.1029/2007JG000547

    Google Scholar 

  • Stokes MA, Smiley TL (1968) An Introduction to Tree Ring Dating. The University of Chicago Press, Chicago

    Google Scholar 

  • Treydte K, Schleser GH, Helle G, Winiger M, Frank DC, Haug GH, Esper J (2006) The twentieth century was the wettest period in northern Pakistan over the past millennium. Nature 440:1179–1182

    Article  Google Scholar 

  • Wada Y (1910) Scientific memoirs of the Korean meteorological observatory, vol 1. Chemulpo, Korea (In Japanese and French)

    Google Scholar 

  • Wang Z, Xu ZB, Li X (1980) The main forest types and their features of community structure in northern slope of Changbai Mountain(in Chinese). Res Forest Ecosyst 1:25–32

    Google Scholar 

  • Wang S, Zhu J, Cai J (2004) Interdecadal variability of temperature and precipitation in China since 1880. Adv Atmos Sci 21(3):307–313

    Article  Google Scholar 

  • Wigley T, Briffa KR, Jones PD (1984) On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. J Appl Meteorol Climatol 23:201–213

    Article  Google Scholar 

  • Xu HC (1990) Pinus tabulaeformis (in Chinese). China Forestry Press, Beijing, pp. 18–23

    Google Scholar 

  • Yao C, Yang S, Qian W, Lin Z, Wen M (2008) Regional summer precipitation events in Asia and their changes in the past decades. J Geophys Res Atmos 113(D17107):1–17. doi:10.1029/2007JD009603

    Google Scholar 

  • Zhang D, Liang Y (2010) A long lasting and extensive drought event over China during 1876-1878. Adv Clim Chang Res 6(2):106–112

    Google Scholar 

  • Zhu HF, Fang XQ, Shao XM, Yin ZY (2009) Tree ring-based February–April temperature reconstruction for Changbai Mountain in Northeast China and its implication for east Asian winter monsoon. Clim Past 5:1–6

    Article  Google Scholar 

Download references

Acknowledgments

This work was funded by the National Natural Science Foundation of China Project 41271066, 31570632, 41571094 and 41601045, and the US National Science Foundation Project AGS-PRF: #1137729. Dr. Steve W. Leavitt helped to improve this work. We thank contributors of Korean tree-ring data.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Zhenju Chen.

Electronic supplementary material

ESM 1

(DOC 689 kb)

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Chen, Z., He, X., Davi, N.K. et al. A 258-year reconstruction of precipitation for southern Northeast China and the northern Korean peninsula. Climatic Change 139, 609–622 (2016). https://doi.org/10.1007/s10584-016-1796-9

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10584-016-1796-9

Keywords

Navigation