Skip to main content
Log in

Variations in annual accumulation recorded in a Laohugou ice core from the northeastern Tibetan Plateau and their relationship with atmospheric circulation

  • Original Article
  • Published:
Environmental Earth Sciences Aims and scope Submit manuscript

Abstract

Annual accumulation was reconstructed for a period from 1960 to 2006 using a 21.2-m ice core from the firn basin of Laohugou (LHG) Glacier No. 12 on the northeastern Tibetan Plateau (TP). Significant periodicity of LHG accumulation variations was identified as a quasi-3-year period in accordance with the oscillation of precipitation in the northwestern China, especially the Hexi Corridor. Furthermore, the relationships of LHG accumulation with atmospheric circulation and moisture sources were investigated. LHG accumulation was positively correlated with the 500-hPa geopotential height and pressure in Central Asia, as well as the autumn Northern Atlantic Oscillation, suggesting that the Westerlies may transport moisture to the LHG region and enhance precipitation. In addition, a negative relationship between LHG accumulation and meridional wind indicated that an intense Mongolian cyclone caused by a strong meridional wind in the region could block Arctic air masses from the LHG region. Moisture fluxes and backward air mass trajectories suggested that moisture might originate from Central Asia, Southern and the inland TP. The relationship between LHG accumulation and atmospheric circulation provides an opportunity to reconstruct the history of atmospheric circulation using a deep ice core record.

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
Fig. 6
Fig. 7
Fig. 8

Similar content being viewed by others

References

  • Allan R, Lindesay J, Parker D (1996) El Nino: southern oscillation and climatic variability. Common wealth Scientific and Industrial Research Organization, Melbourne, p 405. ISBN 9780643058033

    Google Scholar 

  • Alley R, Meese D, Shuman C et al (1993) Abrupt increase in Greenland snow accumulation at the end of Younger Dryas event. Nature 362:527–529

    Article  Google Scholar 

  • An Z, Colman SM, Zhou W et al (2012) Interplay between the Westerlies and Asian monsoon recorded in Lake Qinghai sediments since 32 ka. Sci Rep 2:619

    Google Scholar 

  • Azam M, Wagnon P, Vincent C et al (2014) Processes governing the mass balance of Chhota Shigri Glacier (Western Himalaya, India) assessed by point-scale surface energy balance measurements. Cryosphere 8:2195–2217

    Article  Google Scholar 

  • Bothe O, Fraedrich K, Zhu X et al (2011) Large-scale circulations and Tibetan Plateau summer drought and wetness in a high-resolution climate model. Int J Climatol 31(6):832–846

    Article  Google Scholar 

  • Bryson RA (1986) Airstream climatology of Asia. In: Proceedings of the international symposium on the Qinghai–Xizang Plateau and Mountain Meteorology. American Meteorological Society, Boston, pp 604–617

  • Chen R, Kang E, Zhang J (2001) Application of wavelet transform on annual runoff, yearly average air temperature and annual precipitation periodic variations in Hexi region. Adv Earth Sci 16:339–345

    Google Scholar 

  • Chen D, Cane MA, Kaplan A, Zebiak SE, Huang D (2004) Predictability of El Niño over the past 148 years. Nature 428:733–736

    Article  Google Scholar 

  • Cobb KM, Adkins JF, Partin JW, Clark B (2007) Regional-scale climate influences on temporal variations of rainwater and cave dripwater oxygen isotopes in northern Borneo. Earth Planet Sci Lett 263:207–220

    Article  Google Scholar 

  • Cui X, Ren J, Qin X et al (2011) Climatic and environmental records within a shallow ice core at Laohugou glacier No. 12, Qilian Mountains. J Glaciol Geocryol 33:1251–1258

    Google Scholar 

  • Cuo L, Zhang Y, Wang Q, Zhang L, Zhou B, Hao Z, Su F (2013) Climate change on the northern Tibetan Plateau during 1957–2009: spatial patterns and possible mechanisms. J Clim 26:85–109

    Article  Google Scholar 

  • Curio J, Maussion F, Scherer D (2015) A 12-year high-resolution climatology of atmospheric water transport over the Tibetan Plateau earth system. Dynamics 6:109–124

    Google Scholar 

  • Dansgaard W (1964) Stable isotopes in precipitation Tellus A 16

  • Ding Y, Wang S, Zheng J, et al (2013) Climate in China [M]. Science Press, Beijing, pp 1–557

  • Dong Z, Qin X, Ren J, Qin D, Cui X, Chen J (2013) A 47-year high resolution chemistry record of atmospheric environment change from the Laohugou Glacier No. 12, north slope of Qilian Mountains, China. Quatern Int 313:137–146

    Article  Google Scholar 

  • Du W, Qin X, Sun W, Liu Y, Hou D (2012) Wind characteristics in accumulation area of the Laohugou Glacier No. 12, Qilian Mountains. J Glaciol Geocryol 34:29–36

    Google Scholar 

  • Duan K, Yao T, Wang N, Tian L, Xu B (2008) The difference in precipitation variability between the North and South Tibetan Plateaus. J Glaciol Geocryol 30:726–731

    Google Scholar 

  • Dutta S, Ramanathan A, Linda A, Pottakkal JG, Singh VB, Angchuk T (2015) Glacier mass balance and its significance on the water resource management in the Western Himalayas. Management of water, energy and bio-resources in the era of climate change: emerging issues and challenges. Springer, Berlin, pp 73–83

    Google Scholar 

  • Dyunin A, Anfilofiyev B, Strapilovich M et al (1978) Strong snow-storms, their effect on snow cover and snow accumulation. J Glaciol 19:441–449

    Google Scholar 

  • Feng Q, Li Z, Liu W (2016) Relationship between large scale atmospheric circulation, temperature and precipitation in the Extensive Hexi region, China, 1960–2011. Quatern Int 392:187–196

    Article  Google Scholar 

  • Gao Y, Cuo L, Zhang Y (2014) Changes in moisture flux over the Tibetan Plateau during 1979–2011 and possible mechanisms. J Clim 27:1876–1893

    Article  Google Scholar 

  • Gao Y, Xu J, Chen D (2015) Evaluation of WRF mesoscale climate simulations over the tibetan plateau during 1979–2011. J Clim 28:2823–2841

    Article  Google Scholar 

  • Garg V, College M, Modinagar, et al (2014) Outgoing long wave radiation (OLR) a proxy of convection. Int J Eng Res Manag Techn 1:229–236

    Google Scholar 

  • Guo P, Zhang X, Zhang S, Wang C, Zhang X (2014a) Decadal variability of extreme precipitation days over Northwest China from 1963 to 2012. J Meteorol Res 28:1099–1113

    Article  Google Scholar 

  • Guo X, Feng Q, Wei Y, et al (2014b) An overview of precipitation isotopes over the Extensive Hexi Region in NW China. Arab J Geosci 8:4365–4378

    Article  Google Scholar 

  • Han Y, Fang X, Zhao T et al (2008) Long range trans-Pacific transport and deposition of Asian dust aerosols. J Environ Sci 20:424–428

    Article  Google Scholar 

  • Hou (2011) The application of stable isotopes and geochemical methods on the hydrological processes in the Laohugou Basin[D]. Master thesis of University of Chinese Academy of Sciences, pp 1–70

  • Hou S, Qin D, Yao T et al (2002) Recent change of the ice core accumulation rates on the Qinghai–Tibetan Plateau. Chin Sci Bull 47(20):1746–1749

    Google Scholar 

  • Immerzeel W, Petersen L, Ragettli S, Pellicciotti F (2014) The importance of observed gradients of air temperature and precipitation for modeling runoff from a glacierized watershed in the Nepalese Himalayas. Water Resour Res 50:2212–2226

    Article  Google Scholar 

  • Inceoglua F, Knudsen M, Olsenc J (2016) A continuous ice-core 10Be record from Mongolian mid-latitudes: influences of solar variability and local climate. Earth Planet Sci Lett 437:47–56

    Article  Google Scholar 

  • Jia W, He Y, Li Z et al (2008) Spatio-temporal distribution characteristics of climate change in Qilian Mountains and Hexi Corridor. J Desert Res 28:1151–1155

    Google Scholar 

  • Joswiak D, Yao T, Wu G, Xu B, Zheng W (2010) A 70-year record of oxygen-18 variability in an ice core from the Tanggula Mountains, central Tibetan Plateau. Clim Past 6:219–227

    Article  Google Scholar 

  • Kang S (2011) Atmospheric circulation and glaciochemical records. Encyclopedia of snow, ice and glaciers. Springer, Berlin, pp 75–76

    Chapter  Google Scholar 

  • Kang S, Qin D, Paul AM, Cameron PW, Ren J (2001) Climatic and environmental records from the Far East Rongbuk ice core, Mt. Qomolangma (Mt. Everest). Episodes 24:176–181

    Google Scholar 

  • Kang S, Karl JK, Paul AM, Qin D, Yao T (2002a) Stable-isotopic composition of precipitation over the northern slope of the central Himalaya. J Glaciol 48:519–526

    Article  Google Scholar 

  • Kang S, Mayewski P, Qin D et al (2002b) Glaciochemical records from a Mt. Everest ice core: relationship to atmospheric circulation over Asia. Atmos Environ 36:3351–3361

    Article  Google Scholar 

  • Kang S, Mayewski PA, Yan Y, Qin D, Yao T, Ren J (2003) Dust records from three ice cores: relationships to spring atmospheric circulation over the Northern Hemisphere. Atmos Environ 37:4823–4835

    Article  Google Scholar 

  • Kang S, Qin D, Ren J, Zhang Y, Kaspari S, Mayewski PA, Hou S (2007) Annual accumulation in the Mt. Nyainqentanglha ice core, southern Tibetan Plateau, China: relationships to atmospheric circulation over Asia. Arct Antarct Al Res 39:663–670

    Article  Google Scholar 

  • Kang S, Zhang Y, Zhang Y et al (2010) Variability of atmospheric dust loading over the central Tibetan Plateau based on ice core glaciochemistry. Atmos Environ 44:2980–2989

    Article  Google Scholar 

  • Kang S, Wang F, Morgenstern U (2015) Dramatic loss of glacier accumulation area on the Tibetan Plateau revealed by ice core tritium and mercury records. Cryosphere 9:1213–1222

    Article  Google Scholar 

  • Karthe D, Chalov S, Borchardt D (2015) Water resources and their management in central Asia in the early twenty first century: status, challenges and future prospects. Environ Earth Sci 73:487–499

    Article  Google Scholar 

  • Kaspari S, Mayewski P, Kang S, et al (2007) Reduction in northward incursions of the South Asian monsoon since ~1400 AD inferred from a Mt. Everest ice core. Geophys Res Lett 34:L16701(1–6)

  • Kaspari S, Mayewski PA, Handley M et al (2009) A high-resolution record of atmospheric dust composition and variability since AD 1650 from a Mount Everest ice core. J Clim 22:3910–3925

    Article  Google Scholar 

  • Klein I, Dietz AJ, Gessner U, Galayeva A, Myrzakhmetov A, Kuenzer C (2014) Evaluation of seasonal water body extents in Central Asia over the past 27 years derived from medium-resolution remote sensing data. Int J Appl Earth Obs Geoinf 26:335–349

    Article  Google Scholar 

  • Li J,Cook E,Chen F, et al (2009) Summer monsoon moisture variability over China and Mongolia during the past four centuries. Geophys Res Lett 36:L22705(1–6)

  • Li Z, Gao Y, Wang Y, et al (2015) Can monsoon moisture arrive in the Qilian Mountains in summer? Quat Int 358:113–125

  • Li Z, Gao Y, Wang Y et al (2015a) Can monsoon moisture arrive in the Qilian Mountains in summer? Quatern Int 358:113–125

    Article  Google Scholar 

  • Li X, Ding Y, Yu Z et al (2015b) An 80-year summer temperature history from the Xiao Dongkemadi ice core in the central Tibetan Plateau and its association with atmospheric circulation. J Asian Earth Sci 98:285–295

    Article  Google Scholar 

  • Li B, Chen Y, Chen Z (2016) Why does precipitation in northwest China show a significant increasing trend from 1960 to 2010? Atmos Res 167:275–284

    Article  Google Scholar 

  • Liepert BG (2002) Observed reductions of surface solar radiation at sites in the United States and worldwide from 1961 to 1990. Geophys Res Lett 29:61–64

    Article  Google Scholar 

  • Liu J, Jiang X-G, Zheng X-J, Kang L, Qi F-Y (2004) An intensive Mongolian cyclone genesis induced severe dust storm. TAO 15:1019–1033

    Google Scholar 

  • Lockwood M (2012) Solar influence on global and regional climates. Surv Geophys 33:503–534

    Article  Google Scholar 

  • Lourens L, Tuenter E (2008) The role of variations of the earth's orbital characteristics. In: Letcher TM (ed) Climate Change: observed impacts on Planet Earth. Elsevier, The Netherlands, pp 103–123

    Google Scholar 

  • Ma Y, Sun L, Ding H (2014) Study on the characteristics of long-wave radiation over China Area. Progress in Electromagnetics Research Symposium Proceedings, pp 637–640

  • Meehl GA, Arblaster JM, Branstator G, van Loon H (2008) A coupled air-sea response mechanism to solar forcing in the Pacific region. J Clim 21:2883–2897

    Article  Google Scholar 

  • Morrill C, Overpeck JT, Cole JE (2003) A synthesis of abrupt changes in the Asian summer monsoon since the last deglaciation. Holocene 13:465–476

    Article  Google Scholar 

  • Pfeffer W, Humphrey N (1996) Determination of timing and location of water movement and ice-layer formation by temperature measurements in sub-freezing snow. J Glaciol 42:292–304

    Google Scholar 

  • Pu J, Yao T, Wang N et al (2004) Fluctuations of the glaciers on the Qinghai–Tibetan Plateau during the past century. J Glaciol Geocryol 26:517–522

    Google Scholar 

  • Qian Z, Wu T, Liang X (2001) Feature of mean vertical circulation over the Qinghai–Xizang Plateau and its neighborhood. Chin J Atmos Sci Chin Ed 25:444–454

    Google Scholar 

  • Qin D, Mayewski PA, Cameron PW et al (2000) Evidence for recent climate change from ice cores in the central Himalaya. Ann Glaciol 31:153–158

    Article  Google Scholar 

  • Sheng Y, Liang H (2004) High precipitation in glacial region of high mountains in high Asia: possible cause. J Glaciol Geocryol 26(6):806–809

    Google Scholar 

  • Sperber KR, Annamalai H, Kang I-S et al (2013) The Asian summer monsoon: an intercomparison of CMIP5 vs. CMIP3 simulations of the late 20th century. Clim Dyn 41:2711–2744

    Article  Google Scholar 

  • Stanhill G, Cohen S (2001) Global dimming: a review of the evidence for a widespread and significant reduction in global radiation with discussion of its probable causes and possible agricultural consequences. Agric For Meteorol 107:255–278

    Article  Google Scholar 

  • Stocker T, Qin D, Plattner, GK et al (2013) IPCC, 2013: climate change 2013: the physical science basis. Contribution of working group I to the fifth assessment report of the intergovernmental panel on climate change

  • Strong M, Sharp ZD, Gutzler DS (2007) Diagnosing moisture transport using D/H ratios of water vapor. Geophys Res Lett 34:L03404(1–5)

    Article  Google Scholar 

  • Sun W, Qin X, Ren J et al (2012) The surface Energy Budget in the accumulation zone of the Laohugou glacier No. 12 in the western qilian mountains, China, in summer 2009. Arct Antarct Al Res 44:296–305

    Article  Google Scholar 

  • Tang M (1963) Pressure systems in the mountainous region of western kansu [J]. Acta Meteorol Sin 2:004

    Google Scholar 

  • Tang X, Sun GW, Qian WH (2007) Study on the Northernmost Boundary of East-Asian Summer Monsoon. Meteorological Press, Beijing

    Google Scholar 

  • Tian L, Yao T, Numaguti A (2001) Stable isotope variations in Monsoon Precipitation on the Tibetan Plateau. J Meteorol Soc Jpn 79:959–966

    Article  Google Scholar 

  • Tian L, Yao T, MacClune K, et al (2007) Stable isotopic variations in west China: a consideration of moisture sources. J Geophys Res 112:D10112(1–12)

    Google Scholar 

  • Vicente S, Beguería S, López M, et al (2009) Daily atmospheric circulation events and extreme precipitation risk in northeast Spain: role of the North Atlantic Oscillation, the Western Mediterranean Oscillation, and the Mediterranean Oscillation. J Geophys Res 114:D08106(1–19)

    Google Scholar 

  • Wang S (2007) Research on the precipitation change and its impacts in Hexi area [D]. Lanzhou University

  • Wang C, Cui Y (2006) A study of the stability of the precipitation cycle over Northwest China in the past 50 years [J]. Earth Sci 6:003

    Google Scholar 

  • Wang N, Jiang X, Thompson L et al (2007) Accumulation rates over the past 500 years recorded in ice cores from the Northern and Southern Tibetan Plateau, China. Arct Antarct Alp Res 39(4):671–677

    Article  Google Scholar 

  • Wang H, Chen Y, Chen Z (2013) Spatial distribution and temporal trends of mean precipitation and extremes in the arid region, northwest of China, during 1960–2010. Hydrol Process 27:1807–1818

    Article  Google Scholar 

  • Wild M, Gilgen H, Roesch A et al (2005) From dimming to brightening: decadal changes in solar radiation at Earth’s surface. Science 308:847–850

    Article  Google Scholar 

  • Xu G, Chen T, Liu X (2009) Potential linkages between the moisture variability in the northeastern Qaidam Basin, China, since 1800 and the East Asian summer monsoon as reflected by tree ring δ18O. J Geophys Res 116:09111

    Article  Google Scholar 

  • Yang M, Yao T, Wang H, Tian L, Gou X (2006) Estimating the criterion for determining water vapour sources of summer precipitation on the northern Tibetan Plateau. Hydrol Processes 20:505–513

    Article  Google Scholar 

  • Yang K, Ye B, Zhou D, Wu B, Foken T, Qin J, Zhou Z (2011) Response of hydrological cycle to recent climate changes in the Tibetan Plateau. Clim Change 109:517–534

    Article  Google Scholar 

  • Yang T, Hao X, Shao Q, Xu C-Y, Zhao C, Chen X, Wang W (2012) Multi-model ensemble projections in temperature and precipitation extremes of the Tibetan Plateau in the 21st century. Glob Planet Change 80:1–13

    Article  Google Scholar 

  • Yang K, Wu H, Qin J, Lin C, Tang W, Chen Y (2014) Recent climate changes over the Tibetan Plateau and their impacts on energy and water cycle: a review. Glob Planet Change 112:79–91

    Article  Google Scholar 

  • Yang J, Duan K, Wu J, et al (2015) Effect of data assimilation using WRF-3DVAR for heavy rain prediction on the northeastern edge of the Tibetan Plateau. Adv Meteorol 2015:294589(1–14)

  • Yao T, Xie Z, Wu X et al (1991) Climatic change since the Little Ice Age recorded by Dunde Ice Cap. Sci China (B) 34(6):760–767

    Google Scholar 

  • Yao T, Shi Y, Thompson L (1997) High resolution record of paleoclimate since the Little Ice Age from the Tibetan ice cores. Quatern Int 37:19–23

    Article  Google Scholar 

  • Yao T, Li Z, Thompson LG et al (2006a) 18O records from Tibetan ice cores reveal differences in climatic changes. Ann Glaciol 43:1–7

    Article  Google Scholar 

  • Yao T, Pu J, Liu S (2006b) Changing glaciers in high Asia. [M] Glacier Science and Environmental Change. Blackwell, England, pp 275–282

    Google Scholar 

  • Yao T, Duan K, Xu B et al (2008) Precipitation record since AD 1600 from ice cores on the central Tibetan Plateau. Clim Past 4:175–180

    Article  Google Scholar 

  • Yao T, Masson D, Gao J et al (2013) A review of climatic controls on δ18O in precipitation over the Tibetan Plateau: observations and simulations. Rev Geophys 51:525–548

    Article  Google Scholar 

  • You Q, Kang S, Aguilar E et al (2011) Changes in daily climate extremes in China and their connection to the large scale atmospheric circulation during 1961–2003. Clim Dyn 36:2399–2417

    Article  Google Scholar 

  • You Q, Fraedrich K, Ren G (2012) Inconsistencies of precipitation in the eastern and central Tibetan Plateau between surface adjusted data and reanalysis. Theor Appl Climatol 109:485–496

    Article  Google Scholar 

  • Yu W, Yao T, Lewis S, Tian L, Ma Y, Xu B, Qu D (2014) Stable oxygen isotope differences between the areas to the north and south of Qinling Mountains in China reveal different moisture sources. Int J Climatol 34:1760–1772

    Article  Google Scholar 

  • Zhai P, Zhang X, Wang H, et al (2005) Trends in Total Precipitation and Frequency of Daily Precipitation Extremes over China. J Clim 18:1096–1108

    Article  Google Scholar 

  • Zhang L (2006) Research on the water resources and hydrological cycle of the Qilian Mountain [D]. Master thesis of Lanzhou University, pp 1–52

  • Zhang Y, Kang S, Qin D, Grigholm B, Mayewski PA (2007) Changes in annual accumulation retrieved from Geladaindong ice core and its relationship to atmospheric circulation over the Tibetan Plateau. Chin Sci Bull 52:3261–3266

    Article  Google Scholar 

  • Zhang Y, Tian Q, Gou X et al (2011) Annual precipitation reconstruction since AD 775 based on tree rings from the Qilian Mountains, northwestern China. Int J Climatol 31:371–381

    Article  Google Scholar 

  • Zhang Y, Wang D, Zhai P, Gu G, He J (2013) Spatial distributions and seasonal variations of tropospheric water vapor content over the Tibetan Plateau. J Clim 26:5637–5654

    Article  Google Scholar 

  • Zhou S, Nakawo M, Sakai A, Matsuda Y, Duan K, Pu J (2007) Water isotope variations in the snow pack and summer precipitation at July 1 Glacier, Qilian Mountains in northwest China. Chin Sci Bull 52:2963–2972

    Article  Google Scholar 

  • Zhou T, Yu R, Zhang J et al (2009) Why the western Pacific subtropical high has extended westward since the late 1970s. J Clim 22:2199–2215

    Article  Google Scholar 

Download references

Acknowledgments

This study was supported by the Global Change Research Program of China (2013CBA01801), the Natural Science Foundation of China (41371091, 41401074, and 41121001).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Shichang Kang.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Du, W., Qin, X., Kang, S. et al. Variations in annual accumulation recorded in a Laohugou ice core from the northeastern Tibetan Plateau and their relationship with atmospheric circulation. Environ Earth Sci 75, 845 (2016). https://doi.org/10.1007/s12665-016-5601-x

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s12665-016-5601-x

Keywords

Navigation