珠江流域降雨结构时空演变特征研究
Spatial-Temporal Changes of Precipitation Structure across the Pearl River Basin, China
摘要: 本文利用珠江流域42个站点1960~200546年的日降雨资料,分析了年降雨总量(ATP)、年降雨总天数(ATD)、年降雨强度(ATI)、年平均降雨历时(MWP)以及各降雨历时的发生率和贡献率等降水指标,探讨了各种不同历时降雨的时空演变特征,并运用了改进Mann-Kendall法检验了降雨序列变化的显著性。研究结果表明:1) 珠江流域上游和中部地区降雨量呈现减少趋势,降雨天数在整个流域范围内呈现减少趋势,由此,流域的降雨强度总体上呈现上升趋势,特别是流域的中部和东部地区;2) 流域短历时降雨(2~5 d)的发生率较高,且占总降雨量的比重较大,表明易于出现集中性的降雨,而长历时降雨则出现下降趋势;3) 珠江流域的暴雨多集中在流域东部地区,而且暴雨在短历时降雨事件中的发生率和贡献率都比较高,特别是流域下游的三角洲地区,洪灾风险会显著提高,增加水资源供给的不确定性,加上经济的发展,人口的增加,需水的提高,将为水资源管理与利用带来新的挑战。
Abstract: Daily precipitation data over the Pearl River basin (1960-2005) from 42 rain gauges is used in this article. Precipitation indices such as annual total precipitation amount, annual total rainy days, annual precipitation intensity and annual mean rainy days are defined. These precipitation indices are analyzed using the modified Mann-Kendall method. Results show that: 1) Decreasing trend of precipitation is found mainly in the middle and upper Pearl River basin. Rainy-days are decreasing almost over the entire basin. Thus, the precipitation intensity of Pearl River basin is increasing, particularly in the middle and the eastern parts of the basin; 2) The occurrence and fractional contribution of wet periods with shorter durations (2 - 5 d) are tending to be predominant while longer durations are decreasing in recent decades; 3) Heavy storms are easy to occur in the eastern of the basin during shorter durations. Higher risk of floods and reduction of water yield in the lower basin will increase uncertainty of water supply in the Pearl River Delta and hence pose new challenges for water resources management.
文章引用:彭俊台, 张强, 陈晓宏. 珠江流域降雨结构时空演变特征研究[J]. 水资源研究, 2012, 1(3): 94-102. https://dx.doi.org/10.12677/JWRR.2012.13014

参考文献

[1] ZOLINA, O., SIMMER, C., GULEV, S. K., et al. Changing structure of European precipitation: Longer wet periods leading to more abundant rainfalls. Geophysical Research Letters, 2010, 37(6), Article ID L06704.
[2] TANK, A. M. G. K., KÖNNEN, G. P. Trends in indices of daily temperature and precipitation extremes in Europe, 1946-1999. Journal of Climate, 2003, 16(22): 3665-3680.
[3] GROISMAN, P. Y., KNIGHT, R. W., EASTERLING, D. R., et al. Trends in intense precipitation in the climate record. Journal of Climate, 2005, 18(9): 1326-1350.
[4] MOBERG, A., JONES, P. D., LISTER, D., et al. Indices for daily temperature and precipitation extremes in Europe analyzed for the period 1901-2000. Journal of Geophysical Research- Atmospheres, 2006, 111(D22): 1-25.
[5] GROISMAN, P. Y., KNIGHT, R. W. Prolonged dry episodes over the conterminous united states: New tendencies emerging during the last 40 years. Journal of Climate, 2008, 21(9): 1850-1862.
[6] BROMMER, D. M., CERVENY, R. S. and BALLING, R. C. Characteristics of long-duration precipitation events across the United States. Geophysical Research Letters, 2007, 34(22): 2-6.
[7] ZHANG, Q., XU, C.-Y., CHEN, X., et al. Statistical behaviours of precipitation regimes in China and their links with atmos- pheric circulation 1960-2005. International Journal of Climatol- ogy, 2011, 31(11): 1665-1678.
[8] ZOLINA, O., SIMMER, C., KAPALA, A., et al. Seasonally dependent changes of precipitation extremes over Germany since 1950 from a very dense observational network. Journal of Geophysical Research-Atmospheres, 2008, 113(D6): 1-17.
[9] KUNKEL, K. E., ANDSAGER, K. and EASTERLING, D. R. Long-term trends in extreme precipitation events over the con- terminous United States and Canada. Journal of Climate, 1999 12(8): 2515-2527.
[10] KUNKEL, K. E., EASTERLING, D. R., REDMOND, K., et al. Temporal variations of extreme precipitation events in the United States: 1895-2000. Geophysical Research Letters, 2003 30(17): 1-4.
[11] ZHANG, Q., XU, C.-Y., GEMMER, M., et al. Changing properties of precipitation concentration in the Pearl River basin, China. Stochastic Environmental Research and Risk Assessment, 2009 23(3): 377-385.
[12] ZHANG, Q., XU, C.-Y., BECKER, S., et al. Trends and abrupt changes of precipitation maxima in the Pearl River basin, China. Atmospheric Science Letters, 2009, 10(2): 132-144.
[13] 王兆礼, 陈晓宏, 张灵, 等. 近40年来珠江流域降水量的时空演变特征[J]. 水文, 2006, 26(6): 71-75. Wang zhaoli, Chen xiaohong, Zhang ling, et al. Spatio-temporal change characteristics of precipitation in the Pearl River basin in recent 40 years. Journal of China Hydrology, 2006, 26(6): 71-75. (in Chinese)
[14] WANG, W., CHEN, X., SHI, P., et al. Detecting changes in ex- treme precipitation and extreme streamflow in the Dongjiang River Basin in southern China. Hydrology and Earth System Sciences, 2008, 12(1): 207-221.
[15] MANN, H. B. Nonparametric tests against trend. Econometrica, 1945, 13(3): 245-259.
[16] KENDALL, M., GIBBONS, J. Rank correlation methods. A Charles Griffin Title, 1990.
[17] HAMED, K. H., RAMACHANDRA, R. A. A modified Mann- Kendall trend test for autocorrelated data. Journal of Hydrology, 1998, 204(1-4): 182-196.
[18] MITCHELL, J. M., DZERDZEEVSKII, B. and FLOHN, H. Climate change. WHO Technical Note 79, Geneva: World Me- teorological Organization, 1966: 79.
[19] DAUFRESNE, M., LENGFELLNER, K. and SOMMER, U. Global warming benefits the small in aquatic ecosystems. Pro- ceedings of the National Academy of Sciences, 2009.
[20] ZHANG, Q., JIANG, T., CHEN, Y. D., et al. Changing properties of hydrological extremes in south China: Natural variations or human influences? Hydrological Processes, 2010, 24(11): 1421- 1432.