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A 1556 year-long early summer moisture reconstruction for the Hexi Corridor, Northwestern China

  • Bao YangEmail author
  • Jianglin Wang
  • Jingjing Liu
Research Paper
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Abstract

We report a 1556 year-long tree-ring width chronology for the Hexi Corridor, in the arid Northwestern China, established by applying the signal-free regional curve standardization method to 416 juniper ring-width series. We found that drought in early summer (May–June) is the primary controlling factor for tree growth in this area. We then developed an early summer moisture (i.e., scPDSI) reconstruction from 455 CE to present. Our reconstruction captures multi-centennial scale moisture variations, showing two long-term dry periods during 800–950 CE and 1000–1200 CE, and two long-term wet periods during 1200–1450 CE and 1510–1620 CE. We found strong similarities between hydroclimatic changes in the Hexi Corridor and Qaidam Basin from interannual to centennial timescales; however, at multi-centennial (>300 years) timescales, hydroclimatic variations in the two regions showed significant regional differences. The Hexi Corridor witnessed a generally dry Medieval Climate Anomaly (MCA, here 800–1200 CE) and the drying 20th century, whereas the Qaidam Basin experienced high-precipitation periods during the MCA and 20th century. The different correlation pattern with Northern Hemisphere temperature suggest that the Qaidam Basin will receive more precipitation under global warming, whereas the Hexi Corridor will become dryer in the future.

Keywords

Hexi Corridor Tree-ring index Early-summer Hydroclimate reconstruction 

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Notes

Acknowledgements

We thank the two anonymous reviewers who helped to improve the manuscript with insightful comments. This study was supported by the National Key R & D Program of China (Grant No. 2017YFA0603302), the National Natural Science Foundation of China (Grant Nos. 41520104005, 41602192, 41325008 & 41402157), and the Belmont Forum and JPI-Climate Collaborative Research Action ‘INTEGRATE’ (Grant No. 41661144008). Jianglin Wang also acknowledges the support of the Innovation Promotion Association Foundation of CAS, and the CAS “West Light” Program.

References

  1. Anchukaitis K J, Wilson R, Briffa K R, Büntgen U, Cook E R, D’Arrigo R, Davi N, Esper J, Frank D, Gunnarson B E, Hegerl G, Helama S, Klesse S, Krusic P J, Linderholm H W, Myglan V, Osborn T J, Zhang P, Rydval M, Schneider L, Schurer A, Wiles G, Zorita E. 2017. Last millennium Northern Hemisphere summer temperatures from tree rings: Part II, spatially resolved reconstructions. Quat Sci Rev, 163: 1–22CrossRefGoogle Scholar
  2. Büntgen U, Tegel W, Nicolussi K, McCormick M, Frank D, Trouet V, Kaplan J O, Herzig F, Heussner K U, Wanner H, Luterbacher J, Esper J. 2011. 2500 years of European climate variability and human susceptibility. Science, 331: 578–582CrossRefGoogle Scholar
  3. Briffa K R, Melvin T M. 2011. A closer look at regional curve standardization of tree-ring records: Justification of the need, a warning of some pitfalls, and suggested improvements in its application. In: Hughes M K, Diaz H F, Swetnam T W, eds. Dendroclimatology: Progress and Prospects. New York: SpringerGoogle Scholar
  4. Buckley B M, Anchukaitis K J, Penny D, Fletcher R, Cook E R, Sano M, Canh Nam L, Wichienkeeo A, That MinhT, Hong T M. 2010. Climate as a contributing factor in the demise of Angkor, Cambodia. Proc Natl Acad Sci USA, 107: 6748–6752CrossRefGoogle Scholar
  5. Chen F, Yuan Y, Wei W, Zhang R, Yu S, Shang H, Zhang T, Qin L, Wang H, Chen F. 2013. Tree-ring-based annual precipitation reconstruction for the Hexi Corridor, NW China: Consequences for climate history on and beyond the mid-latitude Asian continent. Boreas, 42: 1008–1021Google Scholar
  6. Chen J, Chen F, Feng S, Huang W, Liu J, Zhou A. 2015. Hydroclimatic changes in China and surroundings during the medieval climate anomaly and Little Ice Age: Spatial patterns and possible mechanisms. Quat Sci Rev, 107: 98–111CrossRefGoogle Scholar
  7. Cook B I, Ault T R, Smerdon J E. 2015. Unprecedented 21st century drought risk in the American Southwest and central plains. Sci Adv, 1: e1400082CrossRefGoogle Scholar
  8. Cook E. 1985. A time-series analysis approach to tree-ring standardization. Doctoral Dissertation. Tucson: The University of ArizonaGoogle Scholar
  9. Cook E R, Anchukaitis K J, Buckley B M, D’Arrigo R D, Jacoby G C, Wright W E. 2010. Asian monsoon failure and megadrought during the last millennium. Science, 328: 486–489CrossRefGoogle Scholar
  10. Cook E R, Briffa K R, Jones P D. 1994. Spatial regression methods in dendroclimatology: A review and comparison of two techniques. Int J Climatol, 14: 379–402CrossRefGoogle Scholar
  11. Cook E R, Briffa K R, Meko D M, Graybill D A, Funkhouser G. 1995. The ‘segment length curse’ in long tree-ring chronology development for palaeoclimatic studies. Holocene, 5: 229–237CrossRefGoogle Scholar
  12. Cook E R, Peters K. 1997. Calculating unbiased tree-ring indices for the study of climatic and environmental change. Holocene, 7: 361–370CrossRefGoogle Scholar
  13. Dai A. 2013. Increasing drought under global warming in observations and models. Nat Clim Change, 3: 52–58CrossRefGoogle Scholar
  14. Deng Y, Gou X, Gao L, Zhao Z, Cao Z, Yang M. 2012. Aridity changes in the eastern Qilian Mountains since AD 1856 reconstructed from treerings. Quat Int, 283: 78–84CrossRefGoogle Scholar
  15. Diaz H F, Trigo R, Hughes M K, Mann M E, Xoplaki E, Barriopedro D. 2011. Spatial and temporal characteristics of climate in Medieval Times revisited. Bull Amer Meteorol Soc, 92: 1487–1500CrossRefGoogle Scholar
  16. Esper J, Cook E R, Krusic P J, Peters K. 2003. Tests of the RCS method for preserving low-frequency variability in long tree-ring chronologies. Tree-Ring Res, 59: 81–98Google Scholar
  17. Esper J, Frank D, Büntgen U, Kirdyanov A. 2009. Influence of pith offset on tree-ring chronology trend. Trace, 7: 205–210Google Scholar
  18. Fang K, Frank D, Zhao Y, Zhou F, Seppä H. 2015. Moisture stress of a hydrological year on tree growth in the Tibetan Plateau and surroundings. Environ Res Lett, 10: 034010CrossRefGoogle Scholar
  19. Fang K, Gou X, Chen F, Li J, D’Arrigo R, Cook E, Yang T, Davi N. 2009. Reconstructed droughts for the southeastern Tibetan Plateau over the past 568 years and its linkages to the Pacific and Atlantic Ocean climate variability. Clim Dyn, 35: 577–585CrossRefGoogle Scholar
  20. Fritts H C. 1976. Tree Rings and Climate. London: Academic PressGoogle Scholar
  21. Gou X, Deng Y, Gao L, Chen F, Cook E, Yang M, Zhang F. 2015a. Millennium tree-ring reconstruction of drought variability in the eastern Qilian Mountains, northwest China. Clim Dyn, 45: 1761–1770CrossRefGoogle Scholar
  22. Gou X, Gao L, Deng Y, Chen F, Yang M, Still C. 2015b. An 850-year treering- based reconstruction of drought history in the western Qilian Mountains of northwestern China. Int J Climatol, 35: 3308–3319CrossRefGoogle Scholar
  23. Graham N E, Ammann C M, Fleitmann D, Cobb K M, Luterbacher J. 2010. Support for global climate reorganization during the “Medieval Climate Anomaly”. Clim Dyn, 37: 1217–1245CrossRefGoogle Scholar
  24. Holmes R. 1983. Computer assisted quality control in tree-ring dating and measurement. Tree-Ring Bull, 43: 69–78Google Scholar
  25. Huang J, Yu H, Dai A, Wei Y, Kang L. 2017. Drylands face potential threat under 2°C global warming target. Nat Clim Change, 7: 417–422CrossRefGoogle Scholar
  26. Huang J, Yu H, Guan X, Wang G, Guo R. 2015. Accelerated dryland expansion under climate change. Nat Clim Change, 6: 166–171CrossRefGoogle Scholar
  27. Huang N E, Shen Z, Long S R, Wu M C, Shih H H, Zheng Q, Yen N C, Tung C C, Liu H H. 1998. The empirical mode decomposition and the Hilbert spectrum for nonlinear and non-stationary time series analysis. Proc R Soc Lond Ser A-Math Phys Eng Sci, 454: 903–995CrossRefGoogle Scholar
  28. Kang S, Yang B, Qin C. 2012. Recent tree-growth reduction in north central China as a combined result of a weakened monsoon and atmospheric oscillations. Clim Change, 115: 519–536CrossRefGoogle Scholar
  29. Li J, Cook E R, D’Arrigo R, Chen F, Gou X. 2008. Moisture variability across China and Mongolia: 1951–2005. Clim Dyn, 32: 1173–1186CrossRefGoogle Scholar
  30. Li J, Shi J, Zhang D D, Yang B, Fang K, Yue P H. 2017. Moisture increase in response to high-altitude warming evidenced by tree-rings on the southeastern Tibetan Plateau. Clim Dyn, 48: 649–660CrossRefGoogle Scholar
  31. Li Q, Liu Y, Nakatsuka T, Fang K, Song H, Liu R, Sun C, Li G, Wang K. 2018. East Asian Summer Monsoon moisture sustains summer relative humidity in the southwestern Gobi Desert, China: Evidence from d18O of tree rings. Clim Dyn, https://doi.org/10.1007/s00382-018-4515-6Google Scholar
  32. Liang E, Shao X, Liu X. 2009. Annual precipitation variation inferred from tree rings since AD 1770 for the Western Qilian Mts., Northern Tibetan Plateau. Tree-Ring Res, 65: 95–103CrossRefGoogle Scholar
  33. Liang E, Leuschner C, Dulamsuren C, Wagner B, Hauck M. 2016a. Global warming-related tree growth decline and mortality on the north-eastern Tibetan plateau. Clim Change, 134: 163–176CrossRefGoogle Scholar
  34. Liang E, Wang Y, Piao S, Lu X, Camarero J J, Zhu H, Zhu L, Ellison A M, Ciais P, Peñuelas J. 2016b. Species interactions slow warming-induced upward shifts of treelines on the Tibetan Plateau. Proc Natl Acad Sci USA, 113: 4380–4385CrossRefGoogle Scholar
  35. Liu Y, An Z, Ma H, Cai Q, Liu Z, Kutzbach J K, Shi J, Song H, Sun J, Yi L, Li Q, Yang Y, Wang L. 2006. Precipitation variation in the northeastern Tibetan Plateau recorded by the tree rings since 850 AD and its relevance to the Northern Hemisphere temperature. Sci China Ser D-Eartn Sci, 49: 408–420CrossRefGoogle Scholar
  36. Liu Y, Sun C, Li Q, Cai Q. 2016. A picea crassifolia tree-ring width-based temperature reconstruction for the Mt. Dongda region, Northwest China, and its relationship to large-scale climate forcing. PLoS ONE, 11: e0160963CrossRefGoogle Scholar
  37. Ljungqvist F C, Krusic P J, Brattström G, Sundqvist H S. 2012. Northern Hemisphere temperature patterns in the last 12 centuries. Clim Past, 8: 227–249CrossRefGoogle Scholar
  38. Ljungqvist F C, Krusic P J, Sundqvist H S, Zorita E, Brattström G, Frank D. 2016. Northern Hemisphere hydroclimate variability over the past twelve centuries. Nature, 532: 94–98CrossRefGoogle Scholar
  39. Melvin T M, Briffa K R. 2008. A “signal-free” approach to dendroclimatic standardisation. Dendrochronologia, 26: 71–86CrossRefGoogle Scholar
  40. Melvin T M, Briffa K R. 2014. CRUST: Software for the implementation of regional chronology standardisation: Part 1. Signal-Free RCS. Dendrochronologia, 32: 7–20CrossRefGoogle Scholar
  41. Mosley-Thompson E, Thompson L G, Dai J, Davis M, Lin P N. 1993. Climate of the last 500 years: High resolution ice core records. Quat Sci Rev, 12: 419–430CrossRefGoogle Scholar
  42. Pederson N, Hessl A E, Baatarbileg N, Anchukaitis K J, Di Cosmo N. 2014. Pluvials, droughts, the Mongol Empire, and modern Mongolia. Proc Natl Acad Sci USA, 111: 4275–4379Google Scholar
  43. Qin C, Yang B, Melvin T M, Fan Z, Zhao Y, Briffa K R. 2013. Radial growth of Qilian Juniper on the Northeast Tibetan Plateau and potential climate associations. PLoS ONE, 8: e79362CrossRefGoogle Scholar
  44. Shao X, Liang E, Huang L, Wang L. 2005. A 1437-year precipitation history from Qilian juniper in the northeastern Qinghai-Tibetan Plateau. PAGES news, 13: 14–15CrossRefGoogle Scholar
  45. Shao X, Xu Y, Yin Z Y, Liang E, Zhu H, Wang S. 2010. Climatic implications of a 3585-year tree-ring width chronology from the northeastern Qinghai-Tibetan Plateau. Quat Sci Rev, 29: 2111–2122CrossRefGoogle Scholar
  46. Sheppard P R, Tarasov P E, Graumlich L J, Heussner K U, Wagner M, wsterle H, Thompson L G. 2004. Annual precipitation since 515 BC reconstructed from living and fossil juniper growth of northeastern Qinghai Province, China. Clim Dyn, 23: 869–881CrossRefGoogle Scholar
  47. Tian Q, Gou X, Zhang Y, Peng J, Wang J, Chen T. 2007. Tree-Ring Based Drought Reconstruction (AD 1855–2001) for the Qilian Mountains, Northwestern China. Tree-Ring Res, 63: 27–36CrossRefGoogle Scholar
  48. van der Schrier G, Barichivich J, Briffa K R, Jones P D. 2013. A scPDSIbased global data set of dry and wet spells for 1901–2009. J Geophys Res-Atmos, 118: 4025–4048CrossRefGoogle Scholar
  49. Wang J, Yang B, Ljungqvist F C, Luterbacher J, Osborn T J, Briffa K R, Zorita E. 2017. Internal and external forcing of multidecadal Atlantic climate variability over the past 1200 years. Nat Geosci, 10: 512–517CrossRefGoogle Scholar
  50. Wang J, Yang B, Qin C, Kang S, He M, Wang Z. 2014. Tree-ring inferred annual mean temperature variations on the southeastern Tibetan Plateau during the last millennium and their relationships with the Atlantic Multidecadal Oscillation. Clim Dyn, 43: 627–640CrossRefGoogle Scholar
  51. Wang W Z, Liu X H, Xu G B, Shao X M, Qin D H, Sun W Z, An W L, Zeng X M. 2013. Moisture variations over the past millennium characterized by Qaidam Basin tree-ring d18O. Chin Sci Bull, 58: 3956–3961CrossRefGoogle Scholar
  52. Wang Z, Yang B, Deslauriers A, Bräuning A. 2015. Intra-annual stem radial increment response of Qilian juniper to temperature and precipitation along an altitudinal gradient in northwestern China. Trees, 29: 25–34CrossRefGoogle Scholar
  53. Wang Z, Yang B, Deslauriers A, Qin C, He M, Shi F, Liu J. 2012. Two phases of seasonal stem radius variations of Sabina przewalskii Kom. in northwestern China inferred from sub-diurnal shrinkage and expansion patterns. Trees, 26: 1747–1757CrossRefGoogle Scholar
  54. Wigley T M L, Briffa K R, Jones P D. 1984. On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. J Clim Appl Meteorol, 23: 201–213CrossRefGoogle Scholar
  55. Wilson R, Anchukaitis K, Briffa K R, Büntgen U, Cook E, D’Arrigo R, Davi N, Esper J, Frank D, Gunnarson B, Hegerl G, Helama S, Klesse S, Krusic P J, Linderholm H W, Myglan V, Osborn T J, Rydval M, Schneider L, Schurer A, Wiles G, Zhang P, Zorita E. 2016. Last millennium northern hemisphere summer temperatures from tree rings: Part I: The long term context. Quat Sci Rev, 134: 1–18CrossRefGoogle Scholar
  56. Wu Z, Huang N E. 2009. Ensemble empirical mode decomposition: A noise assisted data analysis method. Adv Adapt Data Anal, 01: 1–41CrossRefGoogle Scholar
  57. Xu G, Yao H, Dong A. 1997. Climate Change in Arid and Semiarid Regions of China (in Chinese). Beijing: China Meteorological Press. 1–101Google Scholar
  58. Yang B, Bräuning A, Johnson K R, Shi Y. 2002. General characteristics of temperature variation in China during the last two millennia. Geophys Res Lett, 29: 1324Google Scholar
  59. Yang B, He M, Melvin T M, Zhao Y, Briffa K R. 2013. Climate control on tree growth at the upper and lower treelines: A case study in the qilian mountains, Tibetan Plateau. PLoS ONE, 8: e69065CrossRefGoogle Scholar
  60. Yang B, He M, Shishov V, Tychkov I, Vaganov E, Roßsi S, Ljungqvist F C, Bräuning A, Grießinger J. 2017a. New perspective on spring vegetation phenology and global climate change based on Tibetan Plateau tree-ring data. Proc Natl Acad Sci USA, 114: 6966–6971CrossRefGoogle Scholar
  61. Yang B, Qin C, Bräuning A, Burchardt I, Liu J. 2011. Rainfall history for the Hexi Corridor in the arid northwest China during the past 620 years derived from tree rings. Int J Climatol, 31: 1166–1176CrossRefGoogle Scholar
  62. Yang B, Qin C, Wang J, He M, Melvin T M, Osborn T J, Briffa K R. 2014. A 3500-year tree-ring record of annual precipitation on the northeastern Tibetan Plateau. Proc Natl Acad Sci USA, 111: 2903–2908CrossRefGoogle Scholar
  63. Yang B, Sonechkin D M, Datsenko N M, Liu J, Qin C. 2017b. Establishment of a 4650-year-long eigenvalue chronology based on tree-ring cores from Qilian junipers (Juniperus przewalskii Kom.) in Western China. Dendrochronologia, 46: 56–66CrossRefGoogle Scholar
  64. Yin Z Y, Zhu H, Huang L, Shao X. 2016. Reconstruction of biological drought conditions during the past 2847 years in an alpine environment of the northeastern Tibetan Plateau, China, and possible linkages to solar forcing. Glob Planet Change, 143: 214–227CrossRefGoogle Scholar
  65. Zhang P, Cheng H, Edwards R L, Chen F, Wang Y, Yang X, Liu J, Tan M, Wang X, Liu J, An C, Dai Z, Zhou J, Zhang D, Jia J, Jin L, Johnson K R. 2008. A test of climate, sun, and culture relationships from an 1810- year chinese cave record. Science, 322: 940–942CrossRefGoogle Scholar
  66. Zhang Q B, Cheng G, Yao T, Kang X and Hu ang J. 2003. A 2,326-year tree-ring record of climate variability on the northeastern Qinghai-Tibetan Plateau. Geophys Res Lett, 30: 1739–1742Google Scholar
  67. Zhang Q B, Evans M N, Lyu L. 2015. Moisture dipole over the Tibetan Plateau during the past five and a half centuries. Nat Commun, 6: 8062CrossRefGoogle Scholar
  68. Zhang Y, Shao X, Yin Z, Liang E, Tian Q, Xu Y. 2011. Characteristics of extreme droughts inferred from tree-ring data in the Qilian Mountains, 1700–2005. Clim Res, 50: 141–159CrossRefGoogle Scholar

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© Science China Press and Springer-Verlag GmbH Germany, part of Springer Nature 2019

Authors and Affiliations

  1. 1.Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and ResourcesChinese Academy of SciencesLanzhouChina

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