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[1]YE Zhengwei,YIN Peng.Changes of Precipitation Concentration Degree and Precipitation Concentration Period in Flood Season in the Huaihe River Basin[J].Research of Soil and Water Conservation,2018,25(05):295-299.

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Changes of Precipitation Concentration Degree and Precipitation Concentration Period in Flood Season in the Huaihe River Basin

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 25 Number of periods: 2018 05 Page number: 295-299 Column: Public date: 2018-09-06

Title:: Changes of Precipitation Concentration Degree and Precipitation Concentration Period in Flood Season in the Huaihe River Basin

Author(s):: YE Zhengwei, YIN Peng; School of Urban and Environmental Sciences, Huaiyin Normal University, Huaian, Jiangsu 223300, China

Keywords:: Huaihe River Basin; precipitation in flood season; precipitation concentration degree; precipitation concentration period

CLC:: P932;P467

DOI:: -

Abstract:: Precipitation variability is a hot issue in the hydrological cycle field, and it is also the key reference for the flood and drought mitigation and water resources utilization. Daily precipitation data in the flood season of 30 meteorological stations in the Huaihe River Basin (HRB) from 1960 to 2014 were calculated. Based on the calculation of precipitation concentration index, precipitation concentration degree (PCD) and precipitation concentration period (PCP) were analyzed by the trend test methods and the wavelet analysis. The results showed that:(1) the inter-annual variation of precipitation in the HRB was large, it had a very slight increasing trend, less precipitation was observed in 1970s and the 1990s, but more precipitation was found ever since 2000s; (2) the PCD varied with an insignificant decreasing trend, the 1960s and the 1980s were the largest and lowest decades, respectively; an abrupt change of PCD occurred in 1983; the mean PCP occurred in the early July; the PCP was less in 1980s but larger since 1990s, there was an abrupt change in 1990 in the change of PCP; (3) a period of about 2 year could be checked for PCD and a period of about 3~5 years was quite stable from 1991 to 2004, a period of about 6~9 years was stable between 1970 and 1982, and a positive phase period of 4~5 years was significant for the PCD and PCP.

References:: [1] IPCC. Climate change 2007:The physical science basis:Summary for policy makers[M]. Cambridge:Cambridge University Press, 2007.
[2] IPCC. Managing the risks of extreme events and disasters to advance climate change adaptation[M]. Cambridge:Cambridge University Press, 2012.
[3] 汪方,田红.淮河流域1960-2007年极端强降水事件特征[J].气候变化研究进展,2010,6(3):228-229.
[4] 姜爱军,杜银,谢志清,等.中国强降水过程时空集中度气候趋势[J].地理学报,2005,60(6):1007-1014.
[5] 郑永路,钟平安,万新宇,等.淮河流域主汛期极端降水时空特征变异分析[J].南水北调与水利科技,2012,10(5):13-17.
[6] Oliver J E. Monthly precipitation distribution:a comparative index[J]. Prof. Geogr.,1980,32,300-309.
[7] Vergni L, Todisco F. Spatio-temporal variability of precipitation, temperature and agricultural drought indices in Central Italy[J]. Agricultural and Forest Meteorology, 2011,151:301-313.
[8] Coscarelli R, Caloiero T. Analysis of daily and monthly rainfall concentration in southern Italy(Calabria region)[J]. J. Hydrol.,2012,416(3):145-156.
[9] de Luis M, González-Hidalgo J C, Brunetti M, et al. Precipitation concentration changes in Spain 1946-2005[J]. Natural Hazards and Earth System Science, 2011,11:1259-1265.
[10] Martin-Vide J. Spatial distribution of a daily precipitation concentration index in peninsular Spain[J]. International Journal of Climatology, 2004,24:959-971.
[11] 李英杰,延军平,刘永林.秦岭南北气候干湿变化与降水非均匀性的关系[J].干旱区研究,2016,33(3):619-627.
[12] 张录军,钱永甫.长江流域汛期降水集中程度和洪涝关系研究[J].地球物理学报,2004,47(4):622-630.
[13] 张天宇,程炳岩,王记芳,等.华北雨季降水集中度和集中期的时空变化特征[J].高原气象,2007,26(4):843-852.
[14] 佟晓辉,刘向培,贾庆宇,等.1960-2011年中国日降水集中程度的时空变化特征[J].气候与环境研究,2017,22(3):301-314.
[15] 孔锋,方佳毅,刘凡,等.1951-2012年中国降水集中度和集中期的时空格局[J].北京师范大学学报:自然科学版,2015,51(4):404-411.
[16] Zhang Q, Xu C Y, Gemmer M, et al. Changing properties of precipitation concentration in the Pearl River basin, China[J]. Stochastic Environmental Research and Risk Assessment, 2009,23:377-385.
[17] Shi P, Qiao X Y, Chen X, et al. Spatial distribution and temporal trends in daily and monthly precipitation concentration indices in the upper reaches of the Huai River, China[J]. Stochastic Environmental Research and Risk Assessment, 2014,28:201-212.
[18] Shi W L, Yu X Z, Liao W G, et al. Spatial and temporal variability of daily precipitation concentration in the Lancang River basin, China[J]. J. Hydrol.,2013,495:197-207.
[19] 曹永兴,蔡宏珂,向卫国,等.我国西南地区1963-2012年降水集中指数的变化特征[J].西南大学学报:自然科学版,2016,38(10):117-124.
[20] 肖蓓,崔步礼,李东昇,等.黄土高原不同气候区降水时空变化特征[J].中国水土保持科学,2017,15(1):51-61.
[21] 张礼平,张乐飞,曾凡平. ENSO与中国东部夏季降水的关联[J].热带气象学报,2012,28(2):177-186.
[22] 周亮广,戴仕宝.近60年来淮河流域强降雨时空变化特征[J].南水北调与水利科技,2015,13(5):847-852.
[23] 邢万秋,王卫光,吴杨青,等.淮河流域降雨集中度的时空演变规律分析[J].水电能源科学,2011,29(5):1-5.
[24] 李远平,杨太保,马建国.淠河流域汛期降水集中度和集中期的变化特征[J].资源科学,2012,34(3):418-423.
[25] 郑泳杰,张强,陈晓宏,等.1951-2010年淮河流域极端降水区域频率特征及其环流背景[J].武汉大学学报:理学版,2016,62(4):381-388.
[26] 陆苗,高超,姚梦婷,等.淮河流域极端降水概率分布模型及其应用[J].水土保持通报,2016,36(2)197-202.
[27] 叶金印,黄勇,张春莉,等.近50年淮河流域气候变化时空特征分析[J].生态环境学报,2016,25(1):84-91.
[28] 魏凤英.现代气候统计诊断与预测技术[M].北京:气象出版社,2007.
[29] Torrence C, Compo G P. A practical guide to wavelet analysis[J]. Bulletin of the American Meteorological Society, 1998,79:61-78.
[30] Grinsted A, Moore J C, Jevrejeva S. Application of the cross wavelet transform and wavelet coherence to geophysical time series[J]. Nonlinear Processes in Geophysics, 2004,11:561-566.

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