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中长期水文预报及其在平原洪水资源利用中的应用研究
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摘要
中长期水文预报不仅在水库调度、防洪减灾等工作中有重要的作用,而且在洪水资源利用、水权管理等方面也有很重要的意义,因此,中长期水文预报一直是水文工作者深入探讨的课题。近年来,随着计算机技术的发展和新的数学方法的不断涌现,中长期水文预报得到了较快的发展。但是,由于其复杂性和数据资料等因素的制约,中长期水文预报研究仍处在发展阶段,相对于短期水文预报来说,滞后于生产实际的要求。在预报理论研究上,更多注重的是水文系列的统计相关特性,而对物理成因关系关注的相对较少;在预报方法上,对各种方法的有效性研究不够,使现有的方法很难在实践中推广应用;在预报结果的实际应用上,中长期水文预报目前主要是对水资源的宏观调控起一些参考性作用。基于此,本文探讨了基于物理因子分析的中长期水文预报方法,并将预报成果用于指导平原河流洪水资源利用工作。主要研究内容和成果概述如下:
     (1)从水文循环的机理出发,综合分析影响区域水文情势的物理因素,主要包括天文因素、海表温度、以及大气环流等。详细分析了太阳黑子活动情况、日月地三球位置关系、北太平洋海温冷暖变化、ENSO事件以及大气环流因子等物理因素对区域水文情势的影响,为进行基于物理因子分析的中长期水文预报方法研究提供资料准备和理论支持。
     (2)针对现有水旱灾害趋势预测方法无法体现未来洪水发生可能性和量级的缺陷,根据气象因素与水旱灾害的关系,引入随机过程的概念,提出了区域水旱趋势预测的转移概率、太阳活动相位、厄尔尼诺事件等三种方法,推导了相应的计算公式,综合三种方法预测结果得出最终结论。结合东北区水旱灾害史料,分析了其多年来的水旱灾害特征,并对该区2001~2010年水早趋势进行了预测,不仅为水早灾害时域特性的研究探索了一条新的途径,也可在一定程度上为区域洪水资源利用长期规划的制定、洪水风险管理等工作提供有益参考。
     (3)针对中长期水文预报数据资料的数量和种类繁多,数据间关系复杂,难于检索有用信息并组织用于预报的问题,将关联规则数据挖掘分析方法引入到中长期水文预报研究中,研究了中长期径流关联规则模式的提取及预测方法。首先,结合中长期水文预报的特殊性,根据预报目标初选物理影响因子。然后,根据关联规则挖掘算法的要求对数据进行清洗和预处理,构成预报事务数据集。最后,面对预报事务数据集进行关联规则挖掘,提取满足事先设定的最小支持度和最小置信度的强关联规则,解释规则并建立模型进行预测。实例分析证明,该方法在保证一定精度的情况下大大减小了工作量,有助于从海量数据中提取对预报目标有意义的关联规则和模式。
     (4)针对水文中长期预报中单一的定量预报方法精度偏低,稳定性差,不能满足实际生产活动的要求这一情况,提出了定性定量嵌套的多因子神经网络预报模型。利用人工神经网络灵活多变的拓扑结构和强大的非线性逼近能力,基于前期物理影响因子分析作为输入量,通过改变输出节点的个数,先建立定性预报模型,然后在定性预报的基础上建立定量预报模型,最后综合定性预报和定量预报的结果得出结论。实例分析证明,定性定量嵌套的多因子神经网络预报模型不但有一定的物理成因基础,而且可以较好地克服传统使用单一定量预报模型进行预报的盲目性,提高了预报的精度和可靠性。
     (5)在洪水资源利用中,存在的各种未来信息的不确定性是风险的重要来源。中长期预报可以在不同程度上对洪水资源利用系统中各类因素的未来状态进行界定,从而确定面向整个时期引蓄洪水的时机及其后期安全性。本章以白城为例,研究了中长期水文预报在平原河流洪水资源利用中的应用。基于中长期预报成果,并结合考虑时间因素与蓄水状态的河流洪水资源利用二维风险分析模型,以改变各蓄水单元蓄水状态可能带来的后期损失作为主要的风险损失,兼顾时间与蓄水状态两维特性,对洪水资源利用效益和风险损失进行计算,从而得到考虑中长期预报信息的汛期不同时段各蓄水单元引蓄不同洪量的风险率,为洪水资源利用预案制定和实施提供依据。2005、2006年的洪水资源利用实例证明,较高精度的中长期预报成果对该地区洪水资源利用预案制定和实施起到了积极的作用,可最大限度的避减洪水资源利用中的风险和损失,实现最大效益。
     最后,对全文进行了总结,并对有待进一步研究的问题进行了展望。
Medium and long-term hydrological forecasting plays an important role ranging from reservoir operation, flood control yield to disaster mitigation, floodwater resource utilization, water right management, etc. Medium and long-term hydrological forecasting has been researched by many hydrology scientists. With the new techniques of computer and mathematics methods coming out, medium and long-term hydrological forecasting has a fast development. But it is still under development and lagged behind production process compared to short-term forecast because of its complexity and short of hydrologic data. More attention has been paid to statistical properties in hydrological series in the prediction theory study, and less in physics causes analysis. Neglecting the validity of forecasting methods makes the existing methods not effectively popularized and applied, and used only as a reference in macro-control of water resource in practical application. For these reasons, this paper studied on methods of long-term hydrological forecasting based on physics factor analysis and its application in plain flood resource utilization. The main contents and results are as follows:
     (1) Physical factors of regional hydrologic influence are analyzed from the mechanism of hydrological cycle, including astronomical factors, sea surface temperature, atmospheric circulation factors, and so on. Sunspot activity, relations among sun, moon and earth, changes of North Pacific sea surface temperature, ENSO events, atmospheric circulation factors which affect regional hydrological situation are analyzed in this paper. It gives a theoretical support for the study of medium and long-term hydrological forecasting based on physical factors analysis.
     (2) The relationship between the meteorological factors and the flood hazards has been established, considering that the existing forecasting methods can not express the possibility and degree of flood. Three methods for forecasting the trends of floods and droughts are proposed, and the mathematical formulae are derived through the combination of the meteorological and stochastic concepts and methods. These three methods are the shift probability, the phase of the Sun activities, El Nino events. These methods have been used to forecast the future trends of floods and droughts in Northeast China, which have been proved to be a new way to the study of flood hazard time domain characteristics and an effective reference for guiding regional flood utilization and the practical flood risk management.
     (3) Association rules mining is introduced to medium and long-term hydrological forecasting, aiming on the variety and complex relationships of long-term hydrological forecasting data and difficulty search and management for forecasting. The model of long-term hydrological forecasting based on association rules mining is established in this paper. Firstly, forecast factors are selected to constitute the long-term forecast database based on the forecast object considering the characteristics of hydrology forecast. Secondly, the forecast database is established based on data cleaning and pretreatment. Finally, the strong association rules which accord with the min-support and min-confidence are extracted by the method of apriori. Long-term hydrological forecasting model is established based on the strong association rules. A case is studied to validate this new model, and the results reveal that the model can reduce workload and is helpful to finding the interesting strong association rules for the goal of forecasting from massive data.
     (4) Long-term qualitative and quantitative synthesis prediction model has been established based on the variable topological structure of artificial neural network in this paper, because that the quantitative forecasting method has large errors and the qualitative forecasting methods can not satisfy the production process, Firstly, the qualitative forecasting model is established based on physical factors analysis. Secondly, the quantitative forecasting model is established based on changing output node. Finally, conclusions are drawn by combining qualitative and quantitative forecasting results. Two cases are used to validate this new method, and the results reveal that the method is a better way to improve forecasting accuracy and stability than either of the models used separately.
     (5) There are different kinds of future information uncertainty in the flood resource utilization. They are the main resources of risk. The future state about all kinds of input information in the system can be defined in different degree by using the results of medium and long-term hydrological prediction. The paper analyzes the application of long-term runoff forecast in plain flood resource utilization. Therefore, the risk and the loss during the process of flood utilization can be avoided or reduced. The preplan of flood utilization can be made and the risk and the loss during the process of flood utilization can be avoided or reduced as more as possible based on the results of medium-term runoff forecasting. The application examples of 2005 and 2006 show that the higher precision of long-term hydrological forecast play a positive effort in making and actualizing flood resource utilization preplan. The risk and the loss during the process of flood utilization has been avoided and decreased to the greatest extent and the flood utilization has achieved the biggest benefit by applying the medium and long-term hydrological prediction.
     Finally, conclusions are made, and problems for further study are reviewed.
引文
[1]高吉喜,潘英姿,柳海鹰等.区域洪水灾害易损性评价.环境科学研究,2004,17(6):30-34.
    [2]蒋维,金磊.中国城市减灾对策.北京:中国建筑工业出版社,1992.
    [3]水力电力部水文局.中国水资源评价.北京:水利电力出版社,1987.
    [4]张行南,罗健,陈雷.中国洪水灾害危险程度区划.水利学报,2000,(3):1-7.
    [5]彭广,刘立成,刘敏等.洪涝.北京:气象出版社,2003.
    [6]水利电力部.中国历史大洪水.北京:中国书店出版社,1988.
    [7]吴庆洲.对20世纪中国洪灾的回顾.灾害学,2002,17(2):6-9.
    [8]鄂竟平.论控制洪水向洪水管理转变.中国水利,2004,(8):15-21.
    [9]李坤刚.中国洪水与干旱灾害.中国防汛抗旱,2006,(2):14-16.
    [10]王燕生.工程水文学.北京:水利电力出版社,1991.
    [11]陈金荣,范钟秀.中国中长期水文预报的现状与发展趋势.全国水文预报学术讨论会.北京:水利电力出版社,1985.
    [12]水利电力部水文水利调度中心.水文情报预报规范(SD138-85).1985.
    [13]中华人民共和国水利部.水文情报预报规范(SL250-2000).2000.
    [14]陈守煜.中长期水文预报综合分析理论模式与方法.水利学报,1997,(8):15-21.
    [15]黄忠恕,王钦梁,匡奇.北太平洋和青藏高原下垫面热状况与长江流域汛期旱涝关系初步探讨.全国水文预报学术讨论会.北京:水利电力出版社,1985.
    [16]刘清仁.松花江流域水旱灾害发生规律及长期预报研究.水科学进展,1994,5(4):319-327.
    [17]李永康,陈方维,马开玉,陆菊中.长江中下游夏季特大旱涝预测研究.水科学进展,2000,11(3):266-271.
    [18]章淹.致洪暴雨中期预报进展.水科学进展,1995,6(2):162-168.
    [19]王本德.水文中长期预报模糊数学方法.大连:大连理工大学出版社,1993.
    [20]Box G.E.P.,Jenkens G.M.Time Series Analysis:Forecasting and Control.San Francisco:Holden Day,1970.
    [21]冯国章.枯水径流预报德最优模糊划分自激励门限自回归模型.西北农业大学学报,1997,25(2):21-26.
    [22]金菊良,丁晶,魏一鸣.基于遗传算法德门限自回归模型在浅层地下水位预测中的应用.水利学报,1999,(7):230-234.
    [23]陈守煜.模糊水文学.大连理工大学学报,1988,(1):93-97.
    [24]陈守煜.模糊水文学与水资源系统模糊优化原理.大连:大连理工大学出版社,1990.
    [25]陈守煜,周惠成.水文点值预报与分组预报精度评价的一种数学方法.水能技术经济,1986,(1):23-27.
    [26]陈守煜.水文水资源系统模糊识别理论.大连:大连理工大学出版社,1992.
    [27]吴超羽,张文.水文预报的人工神经网络方法.中山大学学报(自然科学版),1994,33(1):79-90.
    [28]钟登华,王仁超,皮钧.水文预报时间序列神经网络模型.水利学报,1995,(2):69-75.
    [29]胡铁松,袁鹏,丁晶.人工神经网络在水文水资源中的应用.水科学进展,1995,6(1):76-82.
    [30]Hsu K.,Gupta H.V.,Sorroshian S.Artificial neural network modeling of the rainfall-runoff process.Water Resource Research,1995,31(10):2517-2530.
    [31]丁晶,邓育仁,安雪松.人工神经前馈(BP)网络模型用作过渡期径流预测的探索.水电站设计,1997,13(2):69-74.
    [32]胡铁松,丁晶.径流长期分级预报的Kohonen网络方法.水电站设计,1997,13(2):24-29.
    [33]冯国章,李佩成.人工神经网络结构对径流预报精度的影响分析.自然资源学报,1998,13(2):169-174.
    [34]刘国东,丁晶.BP网络用于水文预测的几个问题探讨.水利学报,1999,(1):65-69.
    [35]Huang W.,Xu B.,Chan-Hilton A.Forecasting flows in Apalachicola River using neural networks.Hydrological Processes,2004,18(13):2545-2564.
    [36]徐留兴,梁川,秦远清.改进的Elman模型在紫坪铺月径流预测中的应用.四川大学学报(工程科学版),2006,38(3):38-42.
    [37]屈亚玲,周建中,刘芳等.基于改进的Elman神经网络的径流中长期预报.水文,2006,26(1):45-50.
    [38]李正最.谈灰色静态模型与多元线性回归模型的关系.水资源研究,1990,9(1):68-71.
    [39]谢科范.评灰色系统理论.系统工程,1991,9(4):49-52.
    [40]夏军.中长期径流预估的一种灰关联模式与预测方法.水科学进展,1993,4(3):190-197.
    [41]冯平,杨鹏,李润苗.枯水期径流量的中长期预报模式.水利水电技术,1992,(2):6-9.
    [42]陈意平,李小牛.灰色系统理论在水利中的应用及前景.人民珠江,1996,(1):25-27.
    [43]钟桂芳.灰色变基模型在密云水库长期水文预报中的应用.北京水利,1996,(3):47-50.
    [44]牛东晓,邢棉.时间序列的小波神经网络预测模型研究.系统工程理论与实践,1999,(5):89-92.
    [45]王文圣,袁鹏,丁晶.小波分析及其在日径流过程随机模拟中的应用.水利学报,2000,(11):43-47.
    [46]王文圣,丁晶,向红莲.小波分析在水文学中的应用研究及展望.水科学进展,2002,13(4):515-520.
    [47]Breaford P.W.,Seyfried M.S.,Matison T.H.Searching for chaotic dynamic in snowmelt runoff.Water Resources Research,1991,27(6):1005-1010.
    [48]Sivakumar B.,Berndtsson R.,Persson M.Monthly runoff prediction using phase-space reconstruction.Hydrological Sciences Journal,2001,46(3):377-388.
    [49]赵永龙,丁晶,邓育仁.相空间小波网络模型及其在水文中长期预测中的应用.水科学进展,1998,9(3):252-257.
    [50]权先璋,蒋传文,张勇传.径流预报的混沌神经网络理论及应用.武汉城市建设学院学报,1999,16(3):33-37.
    [51]尤卫红,杞明辉,段旭.小波变换在短期气候预测模型研究中的应用.高原气象,1999,18(1):39-46.
    [52]陈南祥,黄强,曹连海等.径流序列的相空间重构神经网络预测模型.河海大学学报(自然科学版),2005,33(5):490-493.
    [53]王博,马跃先,贺北方.月径流序列的多层递阶预报研究.系统工程理论与实践,1999,(7):132-135.
    [54]马体顺,李社宗,赵海青等.用动态时间序列周期分析预测模型作郑州汛期降水预报.河南气象,2006,(2):36-37.
    [55]Liong S Y,Sivapragasm C..Flood stage forecasting with SVM.Jounal of the American Water Resources Association,2002,38(1):173-186.
    [56]李亚伟,陈守煜,韩小军.基于支持向量机SVR的黄河凌汛预报方法.大连理工大学学报,2006,46(2):272-275.
    [57]王景雷,吴景社,孙景生等.支持向量机在地下水位预报中的应用研究.水利学报,2003,(5):122-128.
    [58]王亮,张宏伟,牛志广.支持向量机在城市用水量短期预测中的应用.天津大学学报,2005,38(11):1021-1025.
    [59]张土乔,俞亭超.提高支持向量机洪水峰值预报精度研究.水力发电学报,2005,24(2):35-39.
    [60]林剑艺,程春田.支持向量机在中长期径流预报中的应用.水利学报,2006,37(6):681-686.
    [61]农吉夫,金龙.月平均降水量的二次规划最优组合预测方法研究.热带气象学报,2004,2(6):704-712.
    [62]甘弘.水资源合理配置理论与实践(博士学位论文).北京:中国水利水电科学研究院,2000.
    [63]Buras,N.Scientiflc Allocation of Water Resources.New York:American Elsevier Publication Co.,1972.
    [64]Loucks,D.P.,Stedinger,J.R.And Haith D.A.Water resources systems planning and analysis.New Jersey:Prentice-Hall,Englewood Cliffs,1981.
    [65]Yeh,W.W-G.Reservoir Management and Operations Models:A State-of-the-art Review WaterResources Research,1985,21(12):1797-1818.
    [66]Wardlaw,R.,and M.Sharif.Evaluation of genetic algorithms for optimal reservoir system operation.Water ResourceplanManageASCE,1998,125(1):25-33.
    [67]Dooge.,James C.I.The Emergence of Scientific Hydrology in the Twentieth Century.Advances in Water Science,1999,(9).
    [68]Tissa Illangse Kare,H.J.Morel.Seytowx.Groundwater Modelling(An introduction with Sample Programs in BASIC) 1986.
    [69]I.A.Shiklomanov.World Water Resources and Water Use:Modem Assessment and Outlook for Future.Advances in water Science,1999,(9).
    [70]J.Afzal,D.H.Noble.Optimization model for alternative use of different quality irrigation waters.Journal of Irrigation and Drainage Engineering,1992,118:218-228.
    [71]M.Wang,C.Zhang.Ground water management optimization using genetic algorithms and simulated annealing:Formulation and comparison.Journal of the American Water Resources Association,1998,34(3):519-530.
    [72]V.M.Johnson,L.L.Rogers.Accuracy of network approximators in simulation-optimization.Water Resources Plan Manage,2000,126(2):48-56.
    [73]A.J.Vasquez,R.H.Maier.Achieving water quality system reliability using genetic algorithms Journal of Environmental Engineering,2000,126(10):954-962.
    [74]Morshed,Jahangir,Kaluarachchi.J.Iagath.Enhancements to genetic algorithm for optimal groundwater management.Journal of Hydrologic Engineering,2000,50(1):67-73.
    [75]高波.洪水资源安全利用的理论和实践(博士学位论文).南京:河海大学,2005.
    [76]Miller,B.A.,A.Whitlock,R.C.Hughes.Flood management-The TVA Experience.Water international,1996,21(3):119-130.
    [77]Todorovic P,Zelenhasic E.A stochastic model for flood analysis.Water Resources Research,1970,6(6):1641-1648.
    [78]Todorovic P,Rousselle J.Some problems of flood analysis.Water Resources Research,1971,7(5):1144-1150.
    [79]F.,Wood E.Bayesian approach to analyzing uncertainty among flood frequency models.Water Resources Research,1975,11(6):839-843.
    [80]R,Archer D.Seasonality of flooding and the assessment of flood risk.Proc Inst Civ Eng,1981,70:1023-1035.
    [81]G,Kuczera.On the relationship between the reliability of parameter estimates and hydrologic time series data used in calibration.Water Resources Research,1982,18(1):146-154.
    [82]R,Stedinger J.Design events with specified flood risk.Water Resources Research,1983,19(2):511-522.
    [83]Stedinger J R,Taylor M R.Synthetic stream flow generation 1.Model verification and validation 2Effect of parameter uncertainty.Water Resources Research,1982,18(4):919-924.
    [84]Diaz-Granados M a,Valdes J B,Bras R I.A Physically based flood frequency distribution.Water Resources Research,1984,20(7):995-1002.
    [85]Rasmussen P F,Rosbjerg D..Risk estimation in partial duration series.Water Resources Research,1989,25(11):2319-2330.
    [86]H,Ang a H & Tang W.Probability concepts in engineering planning and design.Decision,Risk and Reliability.New York:Wiley.1984.
    [87]Etal,Simonovic S.P.Risk based parameter selection for shortterm reservoir operation.Journal of Hydrology,1992,131:269-291.
    [88]A,Nardiri.On the integration of risk aversion and average performance optimization in reservoir control.Water Resources Research,1992,28(2):487-497.
    [89]Woube,Mengistu.Flooding and sustainable land-water management in the lower Baro-Akobo river basin,Ethiopia.Applied Geogaphy,1999,(19):235-251.
    [90]涂向阳,高学平,韩延成,郭青平.天津市洪沥水资源化存储研究.自然资源学报,2006,21(3):333-340.
    [91]大连工学院水利系水工教研室,大伙房水库工程管理局.水库控制运用.北京:水利电力出版社,1978.
    [92]大连理工大学,国家防汛抗旱总指挥部办公室.水库防洪预报调度方法及应用.北京:中国水利水电出版社,1996.
    [93]冯平,韩松,李健.水库调整汛限水位的风险效益综合分析.水利学报,2006,37(4):451-456.
    [94]高波,王银堂,胡四一.水库汛限水位调整与运用.水科学进展,2005,16(3):326-333.
    [95]李明宇,谷长叶,董霞等.观音阁-葠窝水库补偿防洪调度汛限水位研究.东北水利水电,2003,(12):34-35.
    [96]殷峻暹,曹永强.基于供水风险分析的汛限水位控制范围研究.水科学进展,2005,16(3):401-405.
    [97]Ji Changming,Liping Wang,Shanyou Feng.A multiobjective reliability programming and decision making method in reservoir system management.Modelling,Measurement &Control,France,1994,44(3):1-11.
    [98]冯平,陈根富.超汛限水位蓄水的风险效益分析.水利学报,1996,(6):29-33.
    [99]傅湘,纪昌明.水库汛期调度的最大洪灾风险率研究.水电能源科学,1998,16(2).
    [100]田峰巍,黄强,解建仓.水库实施调度及风险决策.水利学报,1998,(3):57-62.
    [101]徐玉英,王本德.水库洪水预报子系统的风险分析.水文,2001,21(2):1-4.
    [102]刘俊萍,田峰巍,黄强.水库洪水调度中的风险分析方法.水文,2001,21(3):1-3.
    [103]陈守煜.堤防设计洪水风险分析.黑龙江水专学报,2001,28(4):1-3.
    [104]黄振平,沈福新,朱元甡.基于雨洪预报信息的防洪决策风险分析方法研究.水科学进展,2001,12(4):499-503.
    [105]肖义,郭生练,周芬.基于风险分析的大坝设计洪水标准研究.水力发电,2003,29(11):6-9.
    [106]汪新宇,张翔,赖国伟.防洪体系超标洪水综合风险分析.水利学报,2004,(2):83-87.
    [107]王才君,郭生练,刘攀.三峡水库动态汛限水位洪水调度风险指标及综合评价模型研究.水科学进展,2004,15(3):376-381.
    [108]邱瑞田,王本德,周惠成.水库汛期限制水位控制理论与观念的更新探讨.水科学进展,2004,15(1):68-72.
    [109]王本德,郑德凤,周惠成,马小兵.汛限水位动态控制方案优选方法及指标体系研究.大连理工大学学报,2007,47(1):113-118.
    [110]许士国,刘建卫,陈立羽.通河湖库在洪水资源化中的补偿作用分析.水利学报,2005,36(11):1359-1365.
    [111]许士国,刘建卫,张柏良.洪水资源利用及其风险管理研究.水力发电,2007,33(1):10-13.
    [112]向立云,彭静,张胜红.海河流域蓄滞洪区洪水资源化的示范研究.中国水利水电科学研究院,2003.
    [113]曲兴辉.基于平原水库的水资源调控模式研究(博士学位论文).南京:河海大学,2005.
    [114]高学平,郭磊,李兰秀.蓄滞洪区蓄水优化研究.干旱区资源与环境,2006,20(5):46-50.
    [115]彭静,骆辉煌,马巍,向立云.海河蓄滞洪区洪水资源利用的水污染风险分析.中国水利水电科学研究院学报,2005,3(2):85-90.
    [116]赵飞,王忠静,刘权.洪水资源化与湿地恢复研究.水利水电科技进展,2006,26(1):6-10.
    [117]刘兴土.三江平原沼泽湿地的蓄水与调洪功能.湿地科学,2007,5(1):64-68.
    [118]魏永霞,王丽学.工程水文学.北京:中国水利水电出版社,2005.
    [119]刘伟,范垂仁.中国旱涝巨灾长期预报方法的研究.海洋学报,2005,22(3):11-16.
    [120]马爱生,韩晓明,范垂仁.用天文要素指标预测大洪水.24,2006,5:39-40.
    [121]葛旭阳,朱永禔.青藏高原热力状况异常特征及其与长江中下游地区夏季降水的关系.气象科学,2001,21(2):147-153.
    [122]李跃清.青藏高原地面加热及上空环流场与东侧旱涝预测的关系.大气科学,2003,27(1):107-114.
    [123]范垂仁,顾洪政,曲延光.提高水文长期预测质量的一些做法.吉林水利,2001,(10):8-10.
    [124]范垂仁,李洪尧.暴雨洪水预报方法初探.自然灾害学报,1993,2(3):26-34.
    [125]范垂仁,米晓霞,周曼宇.太阳活动第23周与吉林省洪涝关系.吉林水利,2001,(6):1-4.
    [126]陈功富.日月星辰.长春:长春出版社,2000.
    [127]陈菊英.中国旱涝的分析和长期预报研究.北京:中国农业出版社,1991.
    [128]翁文波.预测学.北京:石油工业出版社,1996.
    [129]赵得秀.论水旱灾害的发生与日食效应的关系.地域研究与开发,1983,(1):13-22.
    [130]冯士筰、李风歧、李少菁.海洋科学导论.北京:高等教育出版社,1999.
    [131]王本德.水文中长期预报模糊数学方法 大连:大连理工大学出版社,1993.
    [132]翟盘茂,李晓燕,任福民.厄尔尼诺.北京:气象出版社,2003.
    [133]M.H.Glantz.变化的洋流:厄尔尼诺对气候与社会的影响.北京:气象出版社,1998.
    [134]刘实,王宁.前期ENSO事件对东北地区夏季气温的影响.热带气象学报,2001,17(3):314-319.
    [135]张庆云,王会军等.中国天气气候异常成因研究-2003年.北京:气象出版社,2004.
    [136]王绍武.气候系统引论.北京:气象出版社,1994.
    [137]丁一.湖北省特大旱涝成因、规律及预报技术.暴雨灾害(三),1999,(2):77-83.
    [138]罗伯良.湖南夏季旱涝与北半球大气环流特征.暴雨灾害(三),1999,(2):55-59.
    [139]黑龙江省水利厅.黑龙江省水旱灾害.哈尔滨:黑龙江省科学技术出版社,1998.
    [140]水利部松辽水利委员会.东北区水旱灾害.长春:吉林人民出版社,2003.
    [141]王平.自然灾害综合区划的研究现状与展望.自然灾害学报,1999,8(1):21-25.
    [142]么枕生.气候统计学基础.北京:科学出版社,1984.
    [143]范垂仁,顾洪政,张文跃.特大旱涝长期定量预测的研究.吉林水利,2001,(2):1-2.
    [144]王绍武,龚道溢.近百年来的ENSO事件及其强度.气象,1999,25(1):9-14.
    [145]水利部松辽水利委员会.东北地区水旱灾害.长春:吉林人民出版社,2003.
    [146]陈玉琼.旱涝灾害指标的研究.灾害学,1989,4(4):10-13.
    [147]Piatetsky-Shapiro G.,Fayyad U.And Smith P.From Data Mining to Knowledge Discovery:an overview.American:AAA/MIT Press,1996.
    [148]J.Han,M.Kambe.Data Mining:Concepts and techniques.San Francisco,CA:Morgaan Kaufrmann Publishers,2001.
    [149]R.Agrawal,T.Imielinski,A.N.Swami.Mining Association Rules between Sets of Items in Large Databases.SIGMOD Conference.1993.
    [150]Han J.,Kamber M.Data Mining:Concepts and Techniques.San Francisco:Academic Press,2001.
    [151]侯雪波,田斌,葛少云,路志英.关联规则技术在电力市场营销分析中的应用.电力系统及其自动化学报,2005,17(2):67-72.
    [152]陆楠,王喆.基于FP-Tree频集模式的FP-Growth算法对关联规则挖掘的影响.吉林大学学报,2003,41(2):180-185.
    [153]周欣,沙朝锋,朱扬勇等.兴趣度-关联规则的又一个阈值.计算机研究与发展,2000,37(5):627-633.
    [154]R.Agrawal,R.Srikant.Fast algorithms for mining association rules.Proceedings of the 20th International Conference on Very Large Database.1994.
    [155]许士国,党连文,牟志录.嫩江1998年特大洪水水环境影响分析.大连理工大学学报,2003,43(1):114-118.
    [156]段元胜.1998年松花江特大洪水分析与防洪策略启示(硕士学位论文).大连:大连理工大学,2005.
    [157]金龙.神经网络气象预报建模理论方法与应用.北京:气象出版社,2004.
    [158]樊琰.组合预测模型在跨流域引水中研究与应用(硕士学位论文).大连:大连理工大学,2006.
    [159]Jin Long,Luo Ying,Lin Zhenshan.Comparison of long-term forecasting of June-August rainfall over Changjiang-Huaihe Vally.Adv Atmos Sin,1997,14(1):87-92.
    [160]郭生练,王金星,彭辉,马绍忠,刘霆.考虑人类活动影响的丰满水库洪水预报方案.水电能源科学,2000,18(2):14-17.
    [161]程春田,王本德,李成林.白山、丰满水库群实时洪水联合调度系统设计与开发.水科学进展,1998,9(1):29-34.
    [162]施能.气象统计预报中的多元分析方法.北京:气象出版社,1992.
    [163]《数学手册》编写组.数学手册.北京:人民出版社,1979.
    [164]刘建卫.平原地区河流洪水资源利用研究(博士学位论文).大连:大连理工大学,2007.
    [165]中国科学院—国家计划委员会自然资源综合考察委员会.中国自然资源手册.北京:科学出版社,1990.
    [166]孔猛.通河水库洪水资源利用研究(硕士学位论文).大连:大连理工大学,2007.

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