Skip to main content
Log in

Hydrologic alteration along the Middle and Upper East River (Dongjiang) basin, South China: a visually enhanced mining on the results of RVA method

  • Original Paper
  • Published:
Stochastic Environmental Research and Risk Assessment Aims and scope Submit manuscript

Abstract

This paper presents a visually enhanced evaluation of the spatio-temporal patterns of the dam-induced hydrologic alteration in the middle and upper East River, south China over 1952–2002, using the range of variability approach (RVA) and visualization package XmdvTool. The impacts of climate variability on hydrological processes have been removed for wet and dry periods, respectively, so that we focus on the impacts of human activities (i.e., dam construction). The results indicate that: (1) along the East River, dams have greatly altered the natural flow regime, range condition and spatial variability; (2) six most remarkable indicators of hydrologic alteration induced by dam-construction are rise rate (1.16), 3-day maximum (0.91), low pulse duration (0.88), January (0.80), July (0.80) and February (0.79) mean flow of the East River during 1952–2002; and (3) spatiotemporal hydrologic alterations are different among three stations along Easter River. Under the influence of dam construction in the upstream, the degree of hydrologic changes from Lingxia, Heyuan to Longchuan station increases. This study reveals that visualization techniques for high-dimensional hydrological datasets together with RVA are beneficial for detecting spatio-temporal hydrologic changes.

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

Similar content being viewed by others

References

  • Bravard JP, Petts GE (1996) Human impacts on fluvial systems. In: Petts GE, Amorros C (eds) Fluvial hydro-systems. Chapman & hall, London, pp 242–262

    Google Scholar 

  • Choi S-U, Yoon B, Woo H (2005) Effects of dam-induced flow regime change on downstream river morphology and vegetation cover in the Hwang River, Korea. River Res Appl 21(2–3):315–325

    Article  Google Scholar 

  • Haan CT (2002) Statistical methods in hydrology. Iowa State University Press, Ames

    Google Scholar 

  • Katrin G (2005) Integrating spatio-temporal information in environmental monitoring data—a visualization approach applied to moss data. Sci Total Environ 347:1–20

    Article  Google Scholar 

  • Keim DA, Kriegel HP (1996) Visualization techniques for mining large databases: a comparison. IEEE Trans Knowl Data Eng 8(6):923–938

    Article  Google Scholar 

  • Kojiri T, Ikebuchi S, Yamada H (1989) Basinwide flood control system by combining prediction and reservoir operation. Stoch Env Res Risk A 3(1):31–49

    Google Scholar 

  • Li ZW, Zhang YK (2008) Multi-scale entropy analysis of Mississippi River flow. Stoch Environ Res Risk A 22(4):507–512

    Article  Google Scholar 

  • Mathlouthi M, Lebdi F (2008) Event in the case of a single reservoir: the Ghèzala dam in Northern Tunisia. Stoch Environ Res Risk A 22:513–528

    Article  Google Scholar 

  • NRC (National Research Council) (1992) Restoration of aquatic systems: science, technology, and public policy. National Academy Press, Washington, DC

    Google Scholar 

  • Petts GE (1979) Complex response of river channel morphology subsequent to reservoir construction. Prog Phys Geogr 3:329–362

    Article  Google Scholar 

  • Petts GE (1980) Long-term consequences of upstream impoundment. Environ Manage 7:325–332

    Google Scholar 

  • Poff LN, Allan JD, Bain MD, Karr JR, Prestegaard KL, Richter BL, Sparks RE, Stromberg JC (1997) The natural flow regime: a paradigm for river conservation and restoration. Bioscience 47:769–784

    Article  Google Scholar 

  • PRWRC (Pearl River Water Resources Commission) (2006) Pearl River Bulletins of 2000, 2001, 2002, 2003, 2004 and 2005. PRWRC website. http://www.pearlwater.gov.cn/. November, 2006 (in Chinese)

  • Reimann C, Kashulina G, Caritat P, Niskavaara HM (2001) Multi-medium regional geochemistry in the European Arctic: element concentration, variation and correlation. Appl Geochem 16:759–780

    Article  CAS  Google Scholar 

  • Richter BD, Richter HE (2000) Prescribing flood regimes to sustain riparian ecosystems along meandering rivers. Conserv Biol 14:1467–1478

    Article  Google Scholar 

  • Richter BD, Baumgartner JV, Powell J, Braun DP (1996) A method for assessing hydrologic alteration within ecosystems. Conserv Biol 10:1163–1174

    Article  Google Scholar 

  • Richter BD, Baumgartner JV, Wigington R, Braun DP (1997) How much water does a river need? Freshw Biol 37:231–249

    Article  Google Scholar 

  • Richter BD, Baumgartner JV, Braun DP, Powell J (1998) A spatial assessment of hydrologic alteration within a river network. Regulated Rivers Res Manage 14:329–340

    Article  Google Scholar 

  • Shi JZ, Chen XH, Wu T (2005) Changing trend of precipitation and stream flow of the Dongjiang River basin and possible causes. Water Resour Power 23(5):8–10 (in Chinese)

    Google Scholar 

  • Stanford JA, Ward JV (1996) Management of aquatic resources in large catchments: recognizing interactions between ecosystem connectivity and environmental disturbance. In: Watershed management: balancing sustainability with environmental change. Springer, New York, pp 91–124

  • Timme HD, Friederike W, Henk V (2005) Quantification strategies for human-induced and natural hydrological changes in wetland vegetation, southern Florida, USA. Quatern Res 64(3):333–342

    Article  Google Scholar 

  • TNC, (The Nature Conservancy) (2001) Indicators of Hydrologic Alteration User’s Manual

  • XmdvTool (1993) Multivariate data visualization tool. http://davis.wpi.edu/~xmdv/

  • Yang T, Zhang Q, Chen YD, Tao X, Xu CY, Chen X (2008) A spatial assessment of hydrologic alteration caused by dam construction in the middle and lower Yellow River, China. Hydrol Processes 22:3829–3843

    Article  Google Scholar 

  • Yoo C (2006) Long term analysis of wet and dry years in Seoul, Korea. J Hydrol 318(1–4):24–36

    Article  Google Scholar 

Download references

Acknowledgments

The work described in this paper was supported by a key grant from the Chinese Ministry of Education (308012), key grant from the National Natural Science Foundation of China (40830639), a grant from the Research Grants Council of the Hong Kong Special Administrative Region, China (CUHK4627/05H), an open research grant from the Key Sediment Lab of the Ministry for Water Resources (2008001), a National Key Technology R&D Program (2007BAC03A060301), and the Program of Introducing Talents of Discipline to Universities—the 111 Project of Hohai University (B08048). Cordial thanks should be extended to the Nature Conservancy, USA for the ‘Indicators of Hydrologic Alteration’ (IHA) software used in RVA computation, the XmdvTool for visualization of high-dimensional hydro-data developed by The University of California, Davis, and the Department of Water Resources and Environment, Sun Yat-sen University for providing hydrologic data of study area. Prof. V. P. Singh from Texas A&M University has kindly read and improved the quality of the final version of the paper.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Tao Yang.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Chen, Y.D., Yang, T., Xu, CY. et al. Hydrologic alteration along the Middle and Upper East River (Dongjiang) basin, South China: a visually enhanced mining on the results of RVA method. Stoch Environ Res Risk Assess 24, 9–18 (2010). https://doi.org/10.1007/s00477-008-0294-7

Download citation

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00477-008-0294-7

Keywords

Navigation