Volume 5 Issue 4
Dec.  2012
Turn off MathJax
Article Contents
Wei ZHANG, Shou-sheng MU, Yan-jing ZHANG, Kai-min CHEN. 2012: Seasonal and interannual variations of flow discharge from Pearl River into sea. Water Science and Engineering, 5(4): 399-409. doi: 10.3882/j.issn.1674-2370.2012.04.004
Citation: Wei ZHANG, Shou-sheng MU, Yan-jing ZHANG, Kai-min CHEN. 2012: Seasonal and interannual variations of flow discharge from Pearl River into sea. Water Science and Engineering, 5(4): 399-409. doi: 10.3882/j.issn.1674-2370.2012.04.004

Seasonal and interannual variations of flow discharge from Pearl River into sea

doi: 10.3882/j.issn.1674-2370.2012.04.004
Funds:  This work was supported by the National Natural Science Foundation of China (Grants No. 41006046 and 51061130545), the Special Fund for Public Welfare Industry of Ministry of Water Resources of China (Grant No. 201301072), the New Teachers’ Fund for Doctor Stations of the Ministry of Education of China (Grant No. 20100094120008), and the Special Fund of State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering of Hohai University (Grants No. 2009586712 and 2009585812).
More Information
  • Corresponding author: Wei ZHANG
  • Received Date: 2011-07-14
  • Rev Recd Date: 2011-11-14
  • Flow discharge from the river basin into the sea has severe impacts on the immediate vicinity of river channels, estuaries, and coastal areas. This paper analyzes the features and temporal trends of flow discharge at Pearl River’s three main gauge stations: the Wuzhou, Shijiao, and Boluo gauge stations on the West River, North River, and East River, respectively. The results show no significant trend in annual mean discharge into the sea at the three gauge stations. Changes of monthly mean discharge at the Boluo Gauge Station are evident, and a majority of monthly discharge in the dry season displays significant increasing trends. Furthermore, changes of the extreme discharge are quite evident, with a significant decreasing trend in the annual maximum discharge and a significant increasing trend in the minimum one. The significantly decreasing ratio of the flood discharge to annual discharge at the Boluo Gauge Station indicates that the flow discharge from the East River has increased in the dry season and decreased in the flood season since the construction of dams and reservoirs. At the other two gauge stations, the Wuzhou and Shijiao gauge stations, the seasonal discharge generally does not change perceptibly. Human impacts, especially those pertaining to reservoir and dam construction, appear to be responsible for the seasonal variation of flow discharge. The results indicate that the construction and operation of dams and reservoirs in the East River have a greater influence on flow discharge, which can well explain why the seasonal variation of flow discharge from the East River is more evident.

     

  • loading
  • Chau, K. W., Wu, C. L., and Li, Y. S. 2005. Comparison of several flood forecasting models in Yangtze River. Journal of Hydrologic Engineering, 10(6), 485-491. [doi: 10.1061/(ASCE)1084-0699(2005)10:6(485)]
    Chen, X. Q., Zong, Y. Q., Zhang, E. F., Xu, J. G., and Li, S. J. 2001. Human impacts on the Changjiang (Yangtze) River basin, China, with special reference to the impacts on the dry season water discharges into the sea. Geomorphology, 41, 111-123.
    Dai, S. B., Yang, S. L., and Cai, A. M. 2008. Impacts of dams on the sediment flux of the Pearl River, southern China. Catena, 76(1), 36-43.
    Kendall, M. G. 1975. Rank Correlation Methods. London: Charles Griffin.
    Lin, J. Y., Cheng, C. T., and Chau, K. W. 2006. Using support vector machines for long-term discharge prediction. Hydrological Sciences Journal, 51(4), 599-612.
    Mann, H. B. 1945. Nonparametric tests against trend. Econometrica, 13(3), 245-259.
    McCarthy, J. J., Canziani, O. F., Leary, N. A., Dokken, D. J., and White, K. S. 2001. Climate Change 2001: Impacts, Adaptation, and Vulnerability. Cambridge: Cambridge University Press.
    Meybeck, M., and Vörösmarty, C. 2005. Fluvial filtering of land-to-ocean fluxes: From natural Holocene variations to Anthropocene. Comptes Rendus Geosciences, 337(1-2), 107-123. [doi:10.1016/ j.crte.2004.09.016]
    Mitchell, J. M., Jr., Dzerdzeevskii, B., Flohn, H., Hofmeyr, W. L., Lamb, H. H., Rao, K. N., and Wallen, C. C. 1966. Climate Change:Report of a Working Group of the Commission for Climatology. Geneva: World Meteorological Organization (WMO).
    Nilsson, C., Reidy, C. A., Dynesius, M., and Revenga, C. 2005. Fragmentation and flow regulation of the world’s large river systems. Science, 308(5720), 405-408. [doi: 10.1126/science.1107887]
    Obasi, G. O. P., and Dowdeswell, E. 1998. Climate Change 1995: IPCC Second Assessment: A Report of the Intergovernmental Panel on Climate Change. Darby: Diane Publishing Co.
    Pearl River Water Resources Committee (PRWRC) 1991. The Pearl River Archive, Vol. 1. Guangzhou: Guangdong Science and Technology Press. (in Chinese)
    Syvitski, J. P. M. 2003. Supply and flux of sediment along hydrological pathways: Research for the 21st century. Global and Planetary Change, 39(1-2), 1-11. [doi: 10.1016/S0921-8181(03)00008-0]
    Syvitski, J. P. M., Vörösmarty, C. J., Kettner, A. J., and Green, P. 2005. Impact of humans on the flux of terrestrial sediment to the global coastal ocean. Science, 308(5720), 376-380. [doi:10.1126/ science.1109454]
    Walling, D. E., and Fang, D. 2003. Recent trends in the suspended sediment loads of the world’s rivers. Global and Planetary Change, 39(1-2), 111-126. [doi: 10.1016/S0921-8181(03)00020-1]
    Wang, H. J., Yang, Z. S., Saito, Y., Liu, J. P., and Sun, X. X. 2006. Interannual and seasonal variation of the Huanghe (Yellow River) water discharge over the past 50 years: Connections to impacts from ENSO events and dams. Global and Planetary Change, 50(3-4), 212-225. [doi:10.1016/ j.gloplacha.2006.01.005]
    Wang, W. C., Chau, K. W., Cheng, C. T., and Qiu, L. 2009. A comparison of performance of several artificial intelligence methods for forecasting monthly discharge time series. Journal of Hydrology, 374(3-4), 294-306. [doi: 10.1016/j.jhydrol.2009.06.019]
    Wu, C. L., Chau, K. W., and Li, Y. S. 2009. Predicting monthly streamflow using data-driven models coupled with data-preprocessing techniques. Water Resources Research, 45, W08432.
    Xu, J. X. 2004. A study of anthropogenic seasonal rivers in China. Catena, 55(1), 17-32. [doi:10.1016/ S0341-8162(03)00089-4]
    Yang, S. L., Gao, A., Hotz, H. M., Zhu, J., Dai, S. B., and Li, M. 2005. Trends in annual discharge from the Yangtze River to the sea (1865-2004). Hydrological Sciences Journal, 50(5), 825-836. [doi:10.1623/ hysj.2005.50.5.825]
    Ye, B. S., Yang, D. Q., and Kane, D. L. 2003. Changes in Lena River streamflow hydrology: Human impacts versus natural variations. Water Resources Research, 39(7), 1-14. [doi: 10.1029/2003WR001991]
    Yue, S., Pilon, P., Phinney, B., and Cavadias, G. 2002. The influence of autocorrelation on the ability to detect trend in hydrological series. Hydrological Processes, 16(9), 1807-1829. [doi: 10.1002/hyp.1095]
    Zhang, Q., Xu C. Y., Becker. S., Zhang, Z. X, Chen, Y. D., and Coulibaly, M. 2009. Trends and abrupt changes of precipitation maxima in the Pearl River Basin, China. Atmospheric Science Letters, 10(2), 132-144. [doi: 10.1002/asl.221]
    Zhang, S. R., Lu, X. X., Higgitt, D. L., Chen, C. T. A., Han, J. T., and Sun, H. G. 2008. Recent changes of water discharge and sediment load in the Zhujiang (Pearl River) Basin, China. Global and Planetary Change, 60(3-4), 365-380. [doi: 10.1016/j.gloplacha.2007.04.003]
    Zhang, X. B., Harvey, K. D., Hogg, W. D., and Yuzyk, T. R. 2001. Trends in Canadian streamflow. Water Resources Research, 37(4), 987-998. [doi: 10.1029/2000WR90035]
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Article Metrics

    Article views (2878) PDF downloads(3974) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return