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Recent tree-growth reduction in north central China as a combined result of a weakened monsoon and atmospheric oscillations

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Abstract

Tree-ring records are a valuable source of information for understanding long-term, regional-scale drought changes. In this study, a tree ring width chronology spanning the last 330 years (A.D. 1681–2010) is developed for the northern fringe of the Asian summer monsoon in north central China based on tree ring widths of the Chinese pine (Pinus tabulaeformis) at three sites in the Hasi Mountain (HSM). An annual (running from the previous August to the present July) Palmer Drought Severity Index (PDSI) series is reconstructed for the period A.D. 1698 to 2010 using a linear regression model. This reconstruction accounts for 49 % of the actual PDSI variance during the calibration period (A.D.1951–2005). During the last past 330 years, the year 1759 drought was the most severe and the 1926–1932 drought was the most long-lasting. These drought episodes resulted in huge economic losses and severe famine. Similar periods of drought are also found in the Great Bend of the Yellow River region, northeastern Tibetan Plateau and northern China. Our drought reconstruction is consistent with the dry-wet index derived from historical documents for the Great Bend of the Yellow River region for the last three centuries, revealing that our annual PDSI reconstruction reflects broad-scale climate anomalies and represents drought variations in the northern fringe of the Asian summer monsoon. The PDSI reconstruction correlates significantly with sea surface temperature (SST) in the eastern equatorial Pacific Ocean and northern Indian Ocean at an annual timescale, implying that El Niño-Southern Oscillation and the Indian monsoon might be influencing drought variability in the study area. Some extremely dry years of 1707, 1764, 1837, 1854, 1878, 1884, 1926 and 1932 coincided with major El Niño events in historical times. The decadal-scale variability is linked to Pacific Decadal Oscillation (PDO) and SST variations in the Atlantic Ocean. The observed recent tree growth reduction is unusual when viewed from a long-term perspective.

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References

  • Allan RJ, Lindesay JA, Parker DE (1996) El Niño Southern Oscillation and climatic variability. CSIRO Publishing, Australia

    Google Scholar 

  • Biondi F, Waikul K (2004) DENDROCLIM2002: a C++ program for statistical calibration of climate signals in tree-ring chronologies. Comput Geosci 30:303–311

    Article  Google Scholar 

  • Bräuning A, Mantwill B (2004) Summer temperature and summer monsoon history on the Tibetan plateau during the last 400 years recorded by tree rings. Geophys Res Lett 31:L24205. doi:24210.21029/22004GL020793

    Article  Google Scholar 

  • Brienen RJW, Lebrija-trejos E, Zuidema PA, Martínez-Ramos M (2010) Climate-growth analysis for a Mexican dry forest tree shows strong impact of sea surface temperatures and predicts future growth declines. Global Change Biol 16:2001–2012

    Article  Google Scholar 

  • Chen M, Xie P, Janowiak JE, Arkin PA (2002) Global land precipitation: a 50-yr monthly analysis based on gauge observations. J Hydrometeorol 3:249–266

    Article  Google Scholar 

  • Chinese Committee of Agricultural Resources Planning (1984) Chinese natural resources planning summary. Science Press, Beijing

    Google Scholar 

  • Cook ER (1985) A time-series analysis approach to tree-ring standardization. Ph.D. Dissertation. The University of Arizona Press, Tucson

  • Cook ER, Kairiukstis A (1990) Methods of dendrochronology: applications in the environmental sciences. Kluwer Academic Press, Dordrecht

    Google Scholar 

  • Cook ER, Peters K (1997) Calculating unbiased tree-ring indices for the study of climatic and environmental change. Holocene 7:361–370

    Article  Google Scholar 

  • Cook ER, Briffa KR, Meko DM, Graybill DA, Funkhouser G (1995) The ‘segment length curse’ in long tree-ring chronology development for palaeoclimatic studies. Holocene 5:229–237

    Article  Google Scholar 

  • Cook ER, Meko DM, Stahle DW, Cleaveland MK (1999) Drought reconstructions for the continental United States. J Clim 12:1145–1162

    Article  Google Scholar 

  • Cook ER, Woodhouse CA, Eakin CM, Meko DM, Stahle DW (2004) Long-term aridity changes in the western United States. Science 306:1015–1018

    Article  Google Scholar 

  • 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

    Article  Google Scholar 

  • Dai AG, Fung IY, Del Genio AD (1997) Surface observed global land precipitation variations during 1900–88. J Clim 10:2943–2962

    Article  Google Scholar 

  • Dai AG, Trenberth KE, Qian T (2004) A global dataset of Palmer Drought Severity Index for 1870–2002: relationship with soil moisture and effects of surface warming. J Hydrometeorol 5:1117–1130

    Article  Google Scholar 

  • Deng YT (1937) History of famine relief in China. Commercial Press, China, 376

    Google Scholar 

  • Easter DR, Evans JL, Groisman PY, Karl KE, Kunkel KE, Ambenje P (2000) Observed variability and trends in extreme climate events: a brief review. B Am Meteorol Soc 81:417–425

    Article  Google Scholar 

  • Esper J, Frank DC, Büntgen U, Verstege A, Luterbacher J, Xoplaki E (2007) Long-term drought severity variations in Morocco. Geophys Res Lett 34. doi:10.1029/2007GL030844

  • Fang K, Gou X, Chen F, Yang M, Li J, He M, Zhang Y, Tian Q, Peng J (2009) Drought variations in the eastern part of northwest China over the past two centuries: evidence from tree rings. Clim Res 38:129–135

    Article  Google Scholar 

  • Feng S, Hu Q (2004) Variations in the teleconnection of ENSO and summer rainfall in northern China: a role of the Indian summer monsoon. J Clim 17:4871–4881

    Article  Google Scholar 

  • Fritts HC (1976) Tree rings and climate. Academic, New York

    Google Scholar 

  • Fu C, Li K (1978) The effects of tropical ocean on the western Pacific subtropical high. Oceanic Selections, No.2, Ocean Press, 16–21

  • Gou X, Chen F, Yang M, Jacoby G, Fang K, Tian Q, Zang Y (2008) Asymmetric variability between maximum and minimum temperatures in Northeastern Tibetan Plateau: evidence from tree rings. Sci China Ser D: Earth Sci 51:41–55

    Article  Google Scholar 

  • Holmes RL (1983) Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bull 43:69–95

    Google Scholar 

  • Hu Q, Feng S (2001) A southward migration of centennial-scale variations of drought/flood in eastern China and the Western United States. J Clim 14:1323–1328

    Article  Google Scholar 

  • Jones PD, Moberg A (2003) Hemispheric and large-scale surface air temperature variations: an extensive revision and an update to 2001. J Clim 16:206–223

    Article  Google Scholar 

  • LeBlanc D, Terrell M (2001) Dendroclimatic analyses using Thornthwaite-Mather-type evapotranspiration models: a bridge between dendroecology and forest simulation models. Tree-ring Re 57:55–66

    Google Scholar 

  • Li K, Chen Y (1979) Some facts about the effect of the meridional difference of SST anomalies of north Pacific on the subtropical high. Sci. Atmos Sin

  • Li J, Gou X, Cook ER, Chen F (2006) Tree-ring based drought reconstruction for the central Tien Shan area, Northwest China. Geophys Res Lett 33:L07715, 1–5

    Article  Google Scholar 

  • Li J, Chen F, Cook ER, Gou X, Zhang Y (2007) Drought reconstruction for north central China from tree rings: the value of the Palmer drought severity index. Int J Climatol 27:903–909

    Article  Google Scholar 

  • Li J, Cook ER, D’Arrigo R, Chen F, Gou X, Peng J, Huang J (2008) Common tree growth anomalies over the northeastern Tibetan Plateau during the last six centuries: implications for regional moisture change. Glob Change Biol 14:2096–2107

    Article  Google Scholar 

  • Liang E, Shao X, Kong Z, Lin J (2003) The extreme drought in the 1920s and its effect on tree growth deduced from tree ring analysis: a case study in North China. Ann For Sci 60:145–152

    Article  Google Scholar 

  • Liang E, Liu X, Yuan Y, Qin N, Fang X, Huang L, Zhu H, Wang L, Shao X (2006) The 1920s drought reconstructed by tree rings and historical documents in the semi-arid and arid areas of northern China. Clim Change 79:403–432

    Article  Google Scholar 

  • Liu HB, Shao XM, Huang L (2002) Reconstruction of early-summer drought indices in mid-north region of China after 1500 using tree ring chronologies. Quat Sci 22:220–229 (in Chinese with English abstract)

    Google Scholar 

  • Liu Y, Cai Q, Shi J (2005a) Seasonal precipitation in the south-central Helan Mountain region, China, reconstructed from tree-ring width for the past 224 years. Can J Forest Res 35:2403–2412

    Article  Google Scholar 

  • Liu Y, Wang L, Shi JF, Cai QF (2005b) Reconstruction of mean drought index from June to August for the last 270 years using tree-ring date in the northern Helan moutain. Quat Sci 25:540–544 (in Chinese with English abstract)

    Google Scholar 

  • López BC, Rodríguez R, Gracia CA, Sabaté S (2006) Climatic signals in growth and its relation to ENSO events of two Prosopis species following a latitudinal gradient in South America. Glob Change Biol 12:897–906

    Article  Google Scholar 

  • Ma Z (2007) The interdecadal trend and shift of dry/wet over the central part of North China and their relationship to the Pacific Decadal Oscillation (PDO). Chin Sci Bull 52:2130–2139

    Article  Google Scholar 

  • Mann ME, Lees J (1996) Robust estimation of background noise and signal detection in climatic time series. Clim Change 33:409–445

    Article  Google Scholar 

  • Michaelsen J (1987) Cross-validation in statistical climate forecast models. J Clim Appl Meteorol 26:1589–1600

    Article  Google Scholar 

  • Minobe S (1997) A 50–70 year climate oscillation over the North Pacific and North America. Geophys Res Lett 24:683–686

    Article  Google Scholar 

  • Osborn TJ, Briffa KR, Jones PD (1997) Adjusting variance for sample-size in tree-ring chronologies and other regional mean time series. Dendrochronologia 15:89–99

    Google Scholar 

  • Palmer WC (1965) Meteorological drought US. Weather Bureau Research Paper 45, Washington, DC, 58 pp

  • Phipps RL (1985) Collecting, preparing, crossdating, and measuring tree increment cores. U.S. Geological Survey Water-Resources Investigations Report, 85–4148

  • Qian WH, Zhu YF (2001) Climate change in China from 1880 to 1998 and its impact on the environmental condition. Clim Change 50:419–444

    Article  Google Scholar 

  • Qian W, Shan X, Chen D (2011) Droughts near the northern fringe of the East Asian summer monsoon in China during 1740–2003. Clim Change. doi::10.1007/s10584-011-0096-7

  • Quinn WH, Neal VT (1992) The historical record of El Nino events. In: Bradley RS, Jones PD (eds) Climate since 1500 AD. Routledge, London, pp 623–648

    Google Scholar 

  • Report D (1995) Report of the damage caused by disaster in China. China Statistical Press, Beijing, pp 1–406

    Google Scholar 

  • Rinn F (2003) TSAP-Win: time series analysis and presentation for dendrochronology and related applications. Version 0.55 User reference. Heidelberg, Germany (http://www.rimatech.com)

  • Schöngart J, Junk WJ, Piedade MTF, Ayres JM, Hüttermann A, Worbes M (2004) Teleconnection between tree growth in the Amazonian floodplains and the El Nino–Southern Oscillation effect. Glob Change Biol 10:683–692

    Article  Google Scholar 

  • Shanxi Committee of Natural Disasters Annals (2002) Historical natural disasters annals. Chinese Meteorological Press, Beijing

    Google Scholar 

  • Shao XM, Xu Y, Yin Z, Liang EY, Zhu H, Wang S (2010) Climatic implications of a 3585-year tree-ring chronology from the northeastern Qinghai-Tibetan Plateau. Quat Sci Rev 29:2111–2122

    Article  Google Scholar 

  • Stokes MA, Smiley TL (1968) An introduction to tree-ring dating. The University of Chicago Press, Chicago

    Google Scholar 

  • Sun M, Wang H (2007) Relationship and its instability of ENSO—Chinese variations in droughts and wet spells. Sci China Ser D: Earth Sci 50:145–152

    Article  Google Scholar 

  • Tan M (2009) Circulation effect: climatic significance of the short term variability of the oxygen isotopes in stalagmites from monsoonal China—dialogue between paleoclimate records and modern climate research. Quat sciences 29:851–862

    Google Scholar 

  • Tourre YM, Rajagopalan B, Kushnir Y (2001) Patterns of coherent decadal and interdecadal climate signals in the Pacific Basin during the 20th Century. Geophys Res Lett 28:2069–2072

    Article  Google Scholar 

  • Trenberth KE, Overpeck JT, Solomon S (2004) Exploring drought and its implications for the future. Eos, Trans-Am Geophys Union 85:27–29

    Article  Google Scholar 

  • Webb RS, Rosenzweig CE, Levine ER (1993) Specifying land surface characteristics in general circulation models: soil profile data set and derived water-holding capacities. Global Biogeochem Cycles 7:97–108

    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 23:201–213

    Article  Google Scholar 

  • Wilhite DA (2000) Drought: a global assessment. Natural Hazards and Disasters Series, Rout-ledge, 700 p

    Google Scholar 

  • Xu G, Yao H, Li X (1997) Climate change in arid and semi-arid regions of China. China Meteorological Press, Beijing

    Google Scholar 

  • Yakir D, Lev-Yadun S, Zangvil A (1996) El Niño and tree growth near Jerusalem over the last 20 years. Global Change Biol 2:97–101. doi:10.1111/j.1365-2486.1996.tb00054

    Article  Google Scholar 

  • Yang B, Qin C, Bräuning A, Burchardt I, Liu J (2010a) Rainfall history for the Hexi Corridor in the arid northwest China during the past 620 years derived from tree rings. Int J Climatol 31:1166–1176. doi:10.1002/joc.2143

    Article  Google Scholar 

  • Yang B, Qin C, Huang K, Fan Z, Liu J (2010b) Spatial and temporal patterns of variations in tree growth over the northeastern Tibetan Plateau during the period AD 1450–2001. Holocene 20:1235–1245. doi:10.1177/0959683610371997

    Article  Google Scholar 

  • Yuan L (1984) The Northwestern Drought and History of the Famine (in Chinese). The People’s Publishing company of Gansu province

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

    Google Scholar 

  • Zhang J, Lin Z (1992) Climate of China. Wiley, New York, 376 p

    Google Scholar 

  • Zhang D, Xue Z (1994) Relationship between the El Niño and precipitation patterns in China since 1500 AD. Q J Appl Meteorol 5:168–175

    Google Scholar 

  • Zhang R, Sumi A, Kimoto M (1999) A diagnostic study of the impact of El Nino on the precipitation in China. Adv Atmos Sci 16:229–241

    Article  Google Scholar 

  • Zhang Y, Gou X, Hu W, Peng J, Liu P (2005) The drought events recorded in tree ring width in Helan Mountain over past 100 years. Acta Ecol Sin 25:2121–2125

    Google Scholar 

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Acknowledgments

The authors extend many thanks to three anonymous reviewers for their thoughtful comments and suggestions. The study was jointly funded by the Chinese Academy of Sciences (CAS) 100 Talents Project (29082762), the National Basic Research Program of China (973 Program) (No. 2010CB950104), the Chinese Academy of Sciences Visiting Professorship for Senior International Scientists (Grant No. 2009S1-38), and the NSFC (Grant No. 41071130, 41002050).

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  1. Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, 320 Donggang West Rd., Lanzhou, Gansu Province, China, 730000

    Shuyuan Kang, Bao Yang & Chun Qin

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  1. Shuyuan Kang
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  2. Bao Yang
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Correspondence to Bao Yang.

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Kang, S., Yang, B. & Qin, C. Recent tree-growth reduction in north central China as a combined result of a weakened monsoon and atmospheric oscillations. Climatic Change 115, 519–536 (2012). https://doi.org/10.1007/s10584-012-0440-6

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