Late Quaternary climatic influences on megalake Jilantai–Hetao, North China, inferred from a water balance model
详细信息    查看全文
  • 作者:Guoxiao Wei ; Zhiguo Rao ; Jun Dong ; Ning Yue ; Huihui Dang…
  • 关键词:Last interglacial ; Jilantai–Hetao basin ; Paleolake ; Water balance model ; Paleoclimate
  • 刊名:Journal of Paleolimnology
  • 出版年:2016
  • 出版时间:March 2016
  • 年:2016
  • 卷:55
  • 期:3
  • 页码:223-240
  • 全文大小:6,913 KB
  • 参考文献:Abbaspour KC, Yang J, Maximov I, Siber R, Bogner K, Mieleitner J, Zobrist J, Srinivasan R (2007) Modelling hydrology and water quality in the pre-alpine/alpine Thur watershed using SWAT. J Hydrol 333:413–430CrossRef
    Arnold JG, Srinivasan R, Muttiah RS, Williams JR (1998) Large area hydrologic modeling and assessment part I: model development. J Am Water Resour Assoc 34:73–89CrossRef
    Bergner AGN, Trauth MH, Bookhagen B (2003) Paleoprecipitation estimates for the Lake Naivasha basin (Kenya) during the last 175 k.y. using a lake-balance model. Glob Planet Change 36:117–136CrossRef
    Bloemendal J, Liu X, Sun Y, Li N (2008) An assessment of magnetic and geochemical indicators of weathering and pedogenesis at two contrasting sites on the Chinese Loess plateau. Palaeogeogr Palaeoclimatol Palaeoecol 257:152–168CrossRef
    Chen FH, Qiang MR, Feng ZD, Wang HB, Bloemendal J (2003) Stable East Asian monsoon climate during the Last Interglacial (Eemian) indicated by paleosol S1 in the western part of the Chinese Loess Plateau. Glob Planet Change 36:171–179CrossRef
    Chen FH, Fan YX, Madsen D, Chun X, Zhao H, Yang LP (2008) Preliminary study on the formation mechanism of the “Jilantai–Hetao” megalake and the lake evolutionary history in Hetao region. Quat Sci 28:866–873 (in Chinese with English Abstract)
    Chen FH, Li GQ, Zhao H, Jin M, Chen X, Fan YX, Liu XK, Wu D, Madsen D (2014) Landscape evolution of the Ulan Buh Desert in northern China during the late Quaternary. Quat Res 81:476–487CrossRef
    China Earthquake Administration (1988) Active faults surrounding the Ordos Plateau. Seismological Press, Beijing, pp 20–75 (in Chinese)
    Darren LF, Luo YZ, Eike L, Zhang MH (2009) Climate change sensitivity assessment of a highly agricultural watershed using SWAT. J Hydrol 374:16–29CrossRef
    Deng QD, You YC (1985) The characteristic and mechanism of tectonic movements to the fault basins surrounding Ordos Plateau. In: Institute of Geology, China Earthquake Administration (ed) Study on the modern movements of the earth’s crust. Seismological Press, Beijing, pp 58–78 (in Chinese)
    Ding ZL, Ren JZ, Yang SL, Liu TS (1999) High-resolution climatic records of the last two glaciations: evidence from loess-soil sequences, north-central China. Quat Sci 1:49–58 (in Chinese with English Abstract)
    Dong GR, Jin HL, Chen HZ, Zhang CL (1998) Geneses of desertification in semiarid and subhumid regions of northern China. Quat Sci 2:136–144 (in Chinese with English Abstract)
    Drogue G, Pfister L, Leviandier T (2004) Simulating the spatio-temporal variability of streamflow response to climate change scenarios in a mesoscale basin. J Hydrol 293:255–269CrossRef
    Fan YX, Chen FH, Wei GX, Madsen DB, Oviatt CG, Zhao H, Chun X, Yang LP, Fan TL, Li GQ (2010) Potential water sources for Late Quaternary Megalake Jilantai–Hetao, China, inferred from mollusk shell 87Sr/86Sr ratios. J Paleolimnol 43:577–587CrossRef
    Ficklin DL, Luo YZ, Luedeling E, Zhang MH (2009) Climate change sensitivity assessment of a highly agricultural watershed using SWAT. J Hydrol 374:16–29CrossRef
    Fréchette B, de Vernal A (2013) Evidence for large-amplitude biome and climate changes in Atlantic Canada during the last interglacial and mid-Wisconsinan periods. Quat Res 79:242–255CrossRef
    Fu GB, Chen SL, Liu CM, Shepard D (2004) Hydro-climatic trends of the Yellow River basin for the last 50 years. Clim Chang 65:149–178CrossRef
    Gassman PW, Reyes MR, Green CH, Arnold JG (2007) The soil and water assessment tool: historical development, applications, and future research directions. Cent Agric Rural Dev Iowa State Univ 50:1211–1250
    Guiot I, Pons A, de Beaulieu JL, Reille M (1989) A 140,000-year continental climate reconstruction from two European pollen records. Nature 338:309–313CrossRef
    Guo XY, Chen FH, Shi Q (2000) The application of GIS and water and energy budget to the study on the water rebuilding of Paleolake: a case in Shiyang River drainage. Sci Geogr Sin 20:422–426 (in Chinese with English Abstract)
    Guo HM, Yang SZ, Tang XH, Li Y, Shen ZL (2008) Groundwater geochemistry and its implications for arsenic mobilization in shallow aquifers of the Hetao basin, Inner Mongolia. Sci Total Environ 393:131–144CrossRef
    IPCC (2007) Climate change 2007: the physical science basis. Contribution of working group I to the fourth assessment report of the intergovernmental panel on climate change. Cambridge University Press, Cambridge, New York
    Jouzel J, Masson-Delmotte V, Cattani O, Dreyfus G, Falourd S, Hoffmann G, Minster B, Nouet J, Barnola JM, Chappellaz J, Fischer H, Gallet JC, Johnsen S, Leuenberger M, Loulergue L, Luethi D, Oerter H, Parrenin F, Raisbeck G, Raynaud D, Schilt A, Schwander J, Selmo E, Souchez R, Spahni R, Stauffer B, Steffensen JP, Stenni B, Stocker TF, Tison JL, Werner M, Wolff EW (2007) Orbital and millennial Antarctic climate variability over the past 800,000 years. Science 317:793–796CrossRef
    Knisel WG (1980) CREAMS: a field scale model for chemicals, runoff, and erosion from agricultural management systems. USDA Conservation Research Report, vol 26, p 643
    Kutzbach JE (1980) Estimates of past climate at Paleolake Chad, North Africa, Based on a hydrological and energy-balance model. Quat Res 14:47–82
    Lea DW, Pak DK, Spero HJ (2000) Climate impact of late Quaternary equatorial Pacific sea surface temperature variations. Science 289:1719–1724CrossRef
    Legates DR, McCabe GJ (1999) Evaluating the use of “goodness-of-fit” measures in hydrologic and hydroclimatic model validation. Water Resour Res 35:233–241CrossRef
    Lettau HH (1969) Evapotranspiration climatonomy. 1. New approach to numerical prediction of monthly evapotranspiration, runoff and soil moisture storage. Res Dev Tech Rep 97:691–699
    Liu Q, McVicar TR (2012) Assessing climate change induced modification of Penman potential evaporation and runoff sensitivity in a large water-limited basin. J Hydrol 464:352–362CrossRef
    Liu Q, Yang Z, Cui B (2008) Spatial and temporal variability of annual precipitation during 1961–2006 in Yellow River Basin, China. J Hydrol 361:330–338CrossRef
    Lü HY (1994) Magnetic susceptibility analysis of modern soil and its implications. Sci China 24:1290–1297 (in Chinese with English Abstract)
    Lü HY, Wu NQ, Liu TS, Han JM, Qin XG, Sun XJ (1996) Seasonal climatic variation recorded by phytolith assemblages from the Baoji loess sequence in central China over the last 150000a. Sci China (Ser D) 39:629–639
    Maher BA, Thompson R (1995) Paleorainfall reconstructions from pedogenic magnetic susceptibility variations in the Chinese loess and paleosols. Quat Res 44:383–391CrossRef
    Maher BA, Thompson R, Zhou LP (1994) Spatial and temporal reconstructions of changes in the Asian palaeomonsoon: a new mineral magnetic approach. Earth Planet Sci Lett 125:461–471CrossRef
    Marra MJ (2003) Last interglacial beetle fauna from New Zealand. Quat Res 59:122–131CrossRef
    Merritt WS, Alila Y, Barton M, Taylor B, Cohen S, Neilsen D (2006) Hydrologic response to scenarios of climate change in sub watersheds of the Okanagan basin, British Columbia. J Hydrol 326:79–108CrossRef
    Musau J, Sang J, Gathenya J, Luedeling E, Home P (2015) SWAT model parameter calibration and uncertainty analysis using the HydroPSO R package in Nzoia Basin, Kenya. J Sustain Res Eng 1:17–29
    Nakayama T (2011) Simulation of the effect of irrigation on the hydrologic cycle in the highly cultivated Yellow River Basin. Agric For Meteorol 151:314–327CrossRef
    Nash JE, Sutcliffe JV (1970) River flow forecasting through conceptual models. Part I: a discussion of principles. J Hydrol 10:282–290CrossRef
    Neitsch SL, Arnold JG, Kiniry JR, Williams JR (2011) Soil and water assessment tool theoretical documentation version 2009. Texas Water Resour Inst Tech, Report No. 406
    Nicholson SE, Yin X (2001) Rainfall conditions in equatorial East Africa during the Nineteenth century as inferred from the record of Lake Victoria. Clim Change 48:387–398CrossRef
    Ning YF, Liu WG, An ZS (2008) A 130-ka reconstruction of precipitation on the Chinese Loess Plateau from organic carbon isotopes. Palaeogeogr Palaeoclimatol Palaeoecol 270:59–63CrossRef
    North Greenland Ice Core Project members (2004) High-resolution record of Northern Hemisphere climate extending into the last interglacial period. Nature 431:147–151CrossRef
    Pan AF, Ma RY, Li RJ (2006) Study on the deep fluid geochemistry in Ordos Basin. Petroleum Industry Press, Beijing (in Chinese)
    Pan BT, Hu ZB, Wang JP, Vandenberghe J, Hu XF (2011) A magnetostratigraphic record of landscape development in the eastern Ordos Plateau, China: transition from Late Miocene and Early Pliocene stacked sedimentation to Late Pliocene and Quaternary uplift and incision by the Yellow River. Geomorphology 125:225–238CrossRef
    Porter SC, Hallet B, Wu X, An Z (2001) Dependence of near-surface magnetic susceptibility on dust accumulation rate and precipitation on the Chinese Loess Plateau. Quat Res 55:271–283CrossRef
    Ren JZ, Ding ZL, Liu DS, Gou ZT, Zhou XQ, Quan H (1998) A window to view climatic instability occurring at northern atlantic ocean from the last interglacial palaeosol in Huining during MIS 5E. Acta Geophys Sin 41:162–167 (in Chinese with English Abstract)
    Schmit C, Rounsevell MD, La Jeunesse I (2006) The limitations of spatial land use data in environmental analysis. Environ Sci Policy 9:174–188CrossRef
    Shuttleworth WJ (1993) Evaporation (chapter 4). In: Maidment DR (ed) Handbook of hydrology. McGraw-Hill, Sydney
    Soil Conservation Service (1984) National engineering handbook. US Department of Agriculture, Washington, DC
    Song FM, Cao ZQ (1994) Primary study on the faults at the eastern piedmont of Bayan Ulan Mountains. Study Act Faults 3:202–205 (in Chinese)
    Sun JM, Diao GY, Wen QZ (1999) A preliminary study on quantitative estimate of palaeoclimate by using geochemical transfer function in the loess plateau. Geochimica 28:265–272 (in Chinese with English Abstract)
    Tachikawa K, Sépulcre S, Toyofuku T, Bard E (2008) Assessing influence of diagenetic carbonate dissolution on planktonic foraminiferal Mg/Ca in the southeastern Arabian Sea over the past 450 ka: comparison between Globigerinoides ruber and Globigerinoides sacculifer. Geochem Geophys Geosyst 9:Q04037
    Van Griensven A, Meixner T, Grunwald S, Bishop T, Diluzio M, Srinivasan R (2006) A global sensitivity analysis tool for the parameters of multi-variable catchment models. J Hydrol 324:10–23CrossRef
    Wang Y, Cheng H, Edwards RL, Kong X, Shao X, Chen S, An Z (2008) Millennial-and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature 451:1090–1093CrossRef
    Winkler WG, Swain AM, Kutzbach JE (1986) Middle Holocene dry period in the northern midwestern United States: lake levels and pollen stratigraphy. Quat Res 25:235–250CrossRef
    Winograd IJ, Landwehr JM, Coplen TB, Sharp WD, Riggs AC, Ludwig KR, Kolesar PT (2006) Devils Hole, Nevada, δ18O record extended to the mid-Holocene. Quat Res 66:202–212CrossRef
    Wu NQ, Lü HY, Sun XJ, Guo ZT, Liu JQ, Han JM (1994) Climate transfer function from opal phytolith and its application in paleoclimate reconstruction of China loess paleosol sequence. Quat Sci 14:270–279 (in Chinese with English Abstract)
    Xu CY, Singh VP (2001) Evaluation and generalization of temperature-based methods for calculating evaporation. Hydrol Process 15:305–319CrossRef
    Yang D, Li C, Hu H, Lei Z, Yang S, Kusuda T, Koike T, Musiake K (2004) Analysis of water resources variability in the Yellow River of China during the last half century using historical data. Water Resour Res 40:W06502
    Yang LP, Chen FH, Chun X, Fan YX, Sun Y, Madsen DB, Zhang XQ (2008) The Jilantai Salt Lake shorelines in Northwestern arid China revealed by remote sensing images. J Arid Environ 72:861–866CrossRef
    Zhang XC, Pan QM (2006) Investigation and assessment of the Yellow River basin water resources. The Yellow River Water Conservancy Press, Zhengzhou, pp 50–94 (in Chinese)
    Zhang JY, Wang GQ (2007) The effect study of climate change on hydrology and water resources. Science Press, Beijing, pp 122–130 (in Chinese)
    Zhang HC, Peng JL, Ma YZ, Chen GJ, Feng ZD, Li B, Wünnemann B (2004) Late quaternary palaeolake levels in Tengger Desert, NW China. Palaeogeogr Palaeoclimatol Palaeoecol 211:45–58CrossRef
  • 作者单位:Guoxiao Wei (1) (2)
    Zhiguo Rao (1) (2)
    Jun Dong (2)
    Ning Yue (2)
    Huihui Dang (2)
    Yang Dong (2)

    1. Key Laboratory of Western China’s Environmental Systems (Ministry of Education), Lanzhou University, 222 South Tianshui Road, Lanzhou, 730000, China
    2. School of Earth and Environmental Sciences, Lanzhou University, 222 South Tianshui Road, Lanzhou, 730000, China
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Environment
    Environment
    Sedimentology
    Climate Change
    Physical Geography
    Hydrobiology
    Geology
  • 出版者:Springer Netherlands
  • ISSN:1573-0417
文摘
Water levels of the lakes in the Jilantai–Hetao basin in the great northern bend of the Yellow River have fluctuated dramatically during the late Quaternary in response to changes in climate and basin morphology. A water balance calculation for various lake elevations of the Jilantai–Hetao paleolake (JHL) is therefore needed to constrain the relative importance of these factors in determining lake level changes. The possible paleolake surface areas and volumes for different paleoshorelines were determined using modern topography. The results indicate that at its highest early shoreline (1080 m), the paleolake was >34,000 km2 in area and had a volume of ~16,000 × 108 m3. A simple lake water balance model (LWBM) indicates that under modern climatic conditions, the Yellow River runoff is insufficient to maintain the paleolakes, even at the lowest elevation (i.e., 1050 m). The water deficit is 130.96 × 108 m3 at an elevation of 1080 m. The results indicate that precipitation would need to increase by 12 % at the present temperature, or that the temperature would need to decrease by 1.8 °C with the present precipitation to produce Yellow River runoff that satisfies the JHL water volumes. The soil and water assessment tool (SWAT) model and LWBM were coupled to model the Yellow River runoff required to maintain the JHL. Considering that the paleolake most likely formed during the last interglacial [marine isotopic stage 5e (MIS 5e)], with a temperature 2–4 °C higher than the present day, approximately 24–42 % more precipitation was required in the Yellow River basin to maintain the paleolake at the 1080 m lake level. Paleoclimatic simulation results indicate a much higher precipitation during MIS 5e than that at the present, and the paleoclimatic conditions of MIS 5e had the potential to form and sustain the JHL. From these results, we conclude that climatic factors were critical in the formation of the largest and oldest paleolake, and that they must be considered in concert with tectonically-driven shifts in the paleolake basin in order to achieve a comprehensive understanding of the history of the JHL.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700