Abstract
We examined climate variability at two timescales for northern Xinjiang, China: one is of the past 500 years using dendrochronology data and the other is of the past 50 years using meteorological station data. The regression models built from the 50-year period were used to reconstruct the climate of the 500-year period. The results indicate that climate underwent many alternating warm–cold and wet–dry periods in the past 500 years. For the 50-year period, we applied the Mann–Kendall jump test to data from 48 meteorological stations to identify possible transition points of temperature and precipitation. For this period, we also analyzed the impacts of latitude, altitude, slope aspect, and human activities on climate variability, aiming to recognize major factors that influence regional climate variability. The results show a warming and wetting trend in the recent 50 years in northern Xinjiang. We determined that natural pattern variability is dominant in the long-term climate variability in the region, but human impacts are non-negligible in the past 50 years. Regional climate variability may be associated with or driven by latitude, altitude, ecosystems, topography, and human activities. The study provides an empirical evidence of the unique regional characteristics of inland river basin in an arid area over the global climate change background.
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References
Beniston M, Rebetez M (1996) Regional behavior of minimum temperatures in Switzerland for the period 1979–1993. Theor Appl Climatol 53:231–243
Borgaonkar HP, Pant GB, Kumar KR (1999) Tree-ring chronologies from western Himalya and their dendroclimatic potential. International Association of Wood Anatomists 20:295–309
Briffa KR, Melvin TM, Vaganov EA, Grudd H et al (2008) Trends in recent temperature and radial tree growth spanning 2000 years across northwest Eurasia. Philos Trans R Soc B 363:2271–2284
Chung U, Choi J, Yun JI (2004) Urbanization effect on the observed change in mean monthly temperatures between 1951–1980 and 1971–2000 in Korea. Clim Chang 66(127):136
Coutts AM, Beringer J, Tapper NJ (2008) Investigating the climatic impact of urban planning strategies through the use of regional climate modeling: a case study for Melbourne, Australia. Int J Climatol 28:1943–1957
Diaz HF, Bradley RS (1997) Temperature variations during the last century at high elevation sites. Clim Chang 36:253–279
Dixon KW, Delworth TL, Knutson TR, Spelman MJ et al (2003) A comparison of climate change simulations produced by two GFDL coupled climate models. G1ob Planet Chang 37:81–102
Esper J, Cook ER, Schweingruber FH (2002) Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability. Science 295:2250–2253
Fang KY et al (2009) Drought variations in the eastern part of northwest China over the past two centuries: evidence from tree rings. C1im Res 38:129–135
Fritts HC (1976) Tree rings and climate. Academic, New York
Gruza G, Rankova E, Razuvaev V, Bulygina O (1999) Indicators of climate change for the Russian Federation. Clim Chang 42:219–242
Hao XM, Chen YN, Li WH (2007) Impact of anthropogenic activities on the hydrologic characters of the mainstream of the Tarim River in Xinjiang during the past 50 years. Environ Geol 52:1365–1375
Hasanean HM, Basset HA (2006) Variability of summer temperature over Egypt. Int J Climatol 26:1619–1634
He YQ, Lu AG, Zhang ZL, Pang HX et al (2005) Seasonal variation of regional warming-up structure across China in the past half century. Clim Res 28:213–219
Holmes JA, Cook ER, Yang B (2009) Climate change over the past 2000 years in western China. Quat Int 194:91–107
IPCC (Intergovernmenta1 Pane1 on Climate Change) (2001) Climate change 2001: the scientific basis. In: Albritton DL, Meira Filho LG (eds) The IPCC Third Assessment Report. Working Group I Report. Cambridge University Press, Cambridge
Jiang FQ, Li XM, Wei BG, Hu RJ (2009) Observed trends of heating and cooling degree-days in Xinjiang Province, China. Theor Appl Climatol 97:349–360
Jones PD, New M, Parker DE, Martin S et al (1999) Surface air temperature and its changes over the past 150 years. Rev Geophys 37:173–199
Lawrimore JH, Peterson TC (2000) Pan evaporation trends in dry and humid regions of the United States. J Hydrometeorol 1:543–546
Li HJ, He Q, Yang Q (2004) Analysis of drift potential in Xinjiang in recent 40 years. J Desert Res 24(6):706–710
Li Q, Liu Y, Cai QF, Sun JV et al (2006) Reconstruction of annual precipitation since 1686 A. D. from Ningwu region, ShanxiI province. Quat Sci 26(6):999–1006
Li JB, Chen FH, Cook ER, Gou XH et al (2007) Drought reconstruction for North Central China from tree rings: the value of the Palmer drought severity index. Int J Climatol 27:903–909
Liang EY, Liu XH, Yuan YJ, Qin NS et al (2006) The 1920s drought recorded by tree rings and historical documents in the semi-arid and arid areas of Northern China. Clim chang 79:403–432
Lischeid G (2006) A decision support system for mountain basin management using sparse data. Geophys Res Abstr 8:04223
Liu XD, Chen BD (2000) Climatic warming in the Tibetan Plateau during recent decades. Int J Climatol 20:1729–1742
Liu X, Yin ZY, Shao X, Qin N (2006a) Temporal trends and variability of daily maximum and minimum, extreme temperature events, and growing season length over the eastern and central Tibetan Plateau during 1961–2003. J Geophys Res 111:D19109
Liu Y et al (2006b) 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 49:408–420
Liu Y, Linderholm HW, Song H, Cai Q et al (2009) Temperature variations recorded in Pinus tabulaeformis tree rings from the southern and northern slopes of the central Qinling Mountains, central China. Boreas 38:285–291
Louis AS (1993) A 2000-year tree ring record of annual temperatures in the Sierra Nevada mountains. Science 259:1433–1436
Lu AG (2009) Impacts of global warming change on patterns of temperature in China. J Mt Sci 6:405–410
Mahlstein I, Knutti R (2010) Regional climate change patterns identified by cluster analysis. Clim Dynam 35:587–600
Mansur SBT, Rahman YSP (2007) Analysis on the spatial and temporal changes of population and its influence factors in Xinjiang in the last 50 years. Hum Geogr 98(6):114–119
Mao WY, Jiang YA, Li JF (2006) Analysis on the linear tendency of precipitation in North Xinjiang. Arid Land Geogr 29(6):797–802
Moberg A, Sonechkin DM, Holmgren K, Datsenko NM et al (2005) Highly variable northern hemisphere temperatures reconstructed from low- and high-resolution proxy data. Nature 433:613–617
Oke TR (1987) Boundary layer climates. Methuen, London
Pepin NC, Losleben ML (2002) Climate change in the Colorado Rocky Mountains: free air versus surface temperature trends. Int J Climatol 22:311–329
Pepin NC, Lundquist JD (2008) Temperature trends at high elevations: patterns across the globe. Geophys Res Lett 35:L14701
Pepin NC, Norris J (2005) An examination of the differences between surface and free air temperature trend at high elevation sites: relationships with cloud cover, snow cover and wind. J Geophys Res 110:D24112
Pepin NC, Seidel DJ (2005) A global comparison of surface and free-air temperatures at high elevations. J Geophys Res 110:D03104
Peterson TC, Golubev VS, Groisman PY (1995) Evaporation losing its strength. Nature 377:687–688
Potchter O, Goldman D, Kadish D, Iluz D (2008) The oasis effect in an extremely hot and arid climate: the case of southern Israel. J Arid Environ 72:1721–1733
Qian WH, Zhu YF (2001) Climate change in China from 1880 to 1998 and its impact on the environmental condition. Clim Chang 50:419–444
Qin J, Yang K, Liang SL, Guo XF (2009) The altitudinal dependence of recent rapid warming over the Tibetan Plateau. Clim Chang 97:321–327
Rehman SFQ (2010) Temperature and rainfall variation over Dhahran, Saudi Arabia, (1970–2006). Int J Climatol 30:445–449
Schweingruber FH, Bräker OU, Schär E (1979) Dendroclimatic studies on conifers from central Europe and Great Britain. Boreas 8:427–452
Shen YJ, Liu CM, Liu M, Zeng Y et al (2010) Change in pan evaporation over the past 50 years in the arid region of China. Hydrol Process 24:225–231
Shi QD, Xiao JD, Pan XL, Lv GH et al (2004) Study on the change of vegetation coverage in Xinjiang since recent 20 years. Arid Zone Res 21(4):389–394
Szeicz JM, Macdonald GM (1996) A 930-year ring-width chronology from moisture-sensitive white spruce (Picea glauca Moench) in the north western Canada. Holocene 6:345–351
Vuille M, Bradley RS (2000) Mean annual temperature trends and their vertical structure in the tropical Andes. Geophys Res Lett 27:3885–3888
Vuille M, Bradley RS, Werner M, Keimig F (2003) 20th century climate change in the tropical Andes: observations and model results. Clim Chang 59:75–99
Wang SU, Ye JL, Gong DY (1998) Climate in China during the little Ice Age. Quat Sci 1:54–64
Whiteman CD, Pospichal BH, Eisecbach SF, Weihs PP et al (2004) Inversion breakup in small Rocky Mountain and Alpine Basins. J Appl Meteorol 43:1069–1082
Wiles GC, Arrigo RD, Jacoby GC (1996) Temperature changes along the Gulf of Alaska and Pacific northwest coast modeled from coastal tree rings. Can J For Res 26:474–481
Wu ZT, Zhang HJ, Crystal MK, Cobb NS (2010) Climate change and human activities: a case study in Xinjiang, China. Clim Chang 99:457–472
Xie H, Ye JS, Liu XM, Chongyi E (2010) Warming and drying trends on the Tibetan Plateau (1971–2005). Theor Appl Climatol 101:241–253
Xu ZX, Chen YN, Li JY (2004) Impact of climate change on water resources in the Tarim River basin. Water Resour Manag 18(5):439–458
Xu JH, Li WH, Ji MH, Lu F et al (2010) A comprehensive approach to characterization of the nonlinearity of runoff in the headwaters of the Tarim River, western China. Hydrol Process 24:136–146
Yang B (2003a) Climate history of the Tibetan plateau during the last two millennia. Adv Earth Sci 18(2):285–291
Yang LM (2003b) Climate change of extreme precipitation in Xinjiang. Acta Geogr Sin 58(4):577–583
Yang YH, Li WH, Wei WS, Hao XM et al (2009) Discrepancy analysis of the climate changes among mountain, plain, oasis, and desert in an inland river area in the northern slope of Tianshan Mountains—a case study of Sangong River Basin. J Glaciol Geocryol 31(6):1094–1100
Yuan YJ, He Q, Yu SL (2004) Features of annual precipitation change in Tianshan mountainous area for the recent 40 years and comparison with those in the southern and northern Xinjiang. Sci Meteorol Sin 24(2):220–226
Yuan YJ, Xie GH, Wei WS, Zhang JB (2005) Similarities and differences between summer temperature changes in Tianshan mountainous region and southern and northern Xinjiang. Meteorol Sci Technol 33(2):152–155
Zhang QB, Cheng GD, Yao TD, Kang XC, Huang JG (2003) A 2,326-year tree-ring record of climate variability on the northeastern Qinghai-Tibetan Plateau. Geophys Res Lett 30(14):1739
Zhang Q, Zhang J, Sun GW, Di XH (2008a) Research on water-vapor distribution in the air over OilJan Mountains. Acta Meteorol Sin 22:107–118
Zhang X, Liu XW, Lu G, Liu ZL (2008b) Spatial–temporal change of precipitation and wet days in Bole region of Xinjiang. Desert Oasis Meteorol 2(3):12–17
Zhang HF, Ouyang ZY, Zheng H, Wang XK (2009) Recent climate trends on the northern slopes of the Tianshan Mountains, Xinjiang, China. J Mt Sci 6:255–265
Acknowledgments
The research is supported by the National Basic Research Program of China (973 Program: 2010CB951003), the National Natural Science Foundation of China (no. 40871059, 40901105), and Western Light Talent Culture Project (no. XBBS200810). The authors wish to thank Dr. Li for his assistance.
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Yang, Y., Chen, Y., Li, W. et al. Climatic change of inland river basin in an arid area: a case study in northern Xinjiang, China. Theor Appl Climatol 107, 143–154 (2012). https://doi.org/10.1007/s00704-011-0467-z
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DOI: https://doi.org/10.1007/s00704-011-0467-z