CN112149893A - Design flood value prediction method and device - Google Patents
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Abstract
本发明提供一种设计洪水值预测方法和装置,涉及水文分析技术领域,该方法包括:获取目标流域的年最大洪峰流量信息序列;依据所述年最大洪峰流量信息序列,获取皮尔逊III型分布的似然函数;依据所述皮尔逊III型分布的似然函数,获取惩罚似然函数;依据所述惩罚似然函数,预测所述目标流域的设计洪水值;输出所述预测的设计洪水值。本发明可以减小预测设计洪水值的误差。
The invention provides a design flood value prediction method and device, and relates to the technical field of hydrological analysis. The method includes: obtaining an information sequence of annual maximum flood peak flow in a target watershed; and obtaining a Pearson type III distribution according to the annual maximum flood peak flow information sequence. According to the likelihood function of the Pearson type III distribution, obtain a penalized likelihood function; according to the penalized likelihood function, predict the design flood value of the target watershed; output the predicted design flood value . The present invention can reduce the error of predicting the design flood value.
Description
技术领域technical field
本发明涉及水文分析技术领域,尤其涉及一种设计洪水值的预测方法和装 置。The present invention relates to the technical field of hydrological analysis, and in particular, to a method and device for predicting design flood values.
背景技术Background technique
自20世纪以来,随着气候的变化,全球范围内气温呈显著上升趋势,极 端水文气象事件的发生频率也多呈增加趋势。人类活动使得流域环境发生了显 著变化,例如:不透水面积随着城镇扩张显著增加,加速产汇流过程;草地、 林地、耕地范围的变化改变了流域内产汇流能力;大量水利工程的兴建影响了 流域的汇流过程。Since the 20th century, with the change of climate, the global temperature has shown a significant upward trend, and the frequency of extreme hydrometeorological events has also increased. Human activities have caused significant changes in the basin environment. For example, the impervious area has increased significantly with urban expansion, accelerating the process of runoff and runoff; changes in the range of grasslands, forests, and cultivated land have changed runoff capacity in the basin; the construction of a large number of water conservancy projects has affected the process of runoff and runoff. The process of confluence of watersheds.
流域洪水在年际上的变化趋势给水利工程设计带来了新的挑战。长久以来, 水利工程在规划设计阶段都需要权衡其经济和安全性,过高估计设计洪水值会 增加不必要的工程投入,而低估设计值则会使工程面临较高风险,因此,预测 洪水值往往决定着一个工程的规模。传统的设计方法假定洪水序列服从一致性 和独立同分布假定,未能考虑当下极端水文气象事件多呈显著变化趋势这一特 征,由于水利工程的规划寿命较长,传统的统计推断方法所得的结论可能无法 在未来环境下得到应用,而参数具有变化特征的非一致性分布模型在最近二十 年间逐渐得到应用。非一致性分布模型的参数能表示为时间项或其他协变量的 函数,在能明确协变量未来变化趋势的条件下,非一致性分布模型的应用可以得到更优的拟合结果。The interannual variation trend of watershed floods brings new challenges to the design of water conservancy projects. For a long time, the water conservancy project needs to weigh its economy and safety in the planning and design stage. Overestimating the design flood value will increase unnecessary engineering investment, while underestimating the design value will make the project face higher risks. Therefore, the predicted flood value will increase. Often determines the scale of a project. The traditional design method assumes that the flood sequence obeys the assumption of consistency and independent and identical distribution, and fails to take into account the fact that most extreme hydrometeorological events present a significant change trend. Due to the long planning life of water conservancy projects, the conclusion obtained by traditional statistical inference methods It may not be possible to apply in future environments, while non-uniform distribution models with changing parameters have been gradually applied in the last two decades. The parameters of the non-uniform distribution model can be expressed as a time term or a function of other covariates. Under the condition that the future trend of covariates can be clarified, the application of the non-uniform distribution model can obtain better fitting results.
目前许多不同的分布模型已广泛的应用于水文频率分析中,其中皮尔逊 III型分布应用较为广泛。在一致性假定下,基于矩法、极大似然法都能得到 分布的参数估计量,但矩法无法应用在非一致性假定下,极大似然法估计非一 致性皮尔逊III型分布时也会得到不合理的解。在极大似然法估计非一致性皮 尔逊III型分布时,需要基于数值方法得到计算结果,但基于数值方法的寻优 过程中,往往会因为寻优过程受到干扰从而得到错误的最优解。可见,目前预 测设计洪水值的误差太大。At present, many different distribution models have been widely used in hydrological frequency analysis, among which the Pearson type III distribution is widely used. Under the assumption of consistency, the parameter estimators of the distribution can be obtained based on the method of moments and the maximum likelihood method, but the method of moments cannot be applied under the assumption of non-uniformity. The maximum likelihood method estimates the non-uniform Pearson type III distribution also get unreasonable solutions. When the maximum likelihood method is used to estimate the non-uniform Pearson type III distribution, it is necessary to obtain the calculation results based on the numerical method. However, in the optimization process based on the numerical method, the optimal solution is often obtained because the optimization process is disturbed and the wrong optimal solution is obtained. . It can be seen that the error in predicting the design flood value is too large at present.
发明内容SUMMARY OF THE INVENTION
本发明实施例提供一种设计洪水值预测方法和装置,以解决设计洪水值预 测的问题。Embodiments of the present invention provide a design flood value prediction method and device to solve the problem of design flood value prediction.
第一方面,本发明实施例提供一种设计洪水值预测方法,包括:In a first aspect, an embodiment of the present invention provides a design flood value prediction method, including:
获取目标流域的年最大洪峰流量信息序列;Obtain the annual maximum flood peak flow information sequence of the target watershed;
依据所述年最大洪峰流量信息序列,获取皮尔逊III型分布的似然函数;Obtain the likelihood function of the Pearson III distribution according to the maximum flood peak flow information sequence in the year;
依据所述皮尔逊III型分布的似然函数,获取惩罚似然函数;Obtain a penalty likelihood function according to the likelihood function of the Pearson III distribution;
依据所述惩罚似然函数,预测所述目标流域的设计洪水值;predicting the design flood value of the target watershed according to the penalized likelihood function;
输出所述预测的设计洪水值。The predicted design flood value is output.
第二方面,本发明实施例提供一种设计洪水值预测装置,包括:In a second aspect, an embodiment of the present invention provides a design flood value prediction device, including:
第一获取模块用于获取目标流域的年最大洪峰流量信息序列;The first acquisition module is used to acquire the annual maximum flood peak flow information sequence of the target watershed;
第二获取模块用于依据所述年最大洪峰流量信息序列,获取皮尔逊III型 分布的似然函数;The second acquisition module is used to obtain the likelihood function of Pearson III distribution according to the maximum flood peak flow information sequence of the year;
第三获取模块用于依据所述皮尔逊III型分布的似然函数,获取惩罚似然 函数;The 3rd acquisition module is used to obtain the penalty likelihood function according to the likelihood function of the Pearson III distribution;
第四获取模块用于依据所述惩罚似然函数,预测所述目标流域的设计洪水 值;The fourth acquisition module is used to predict the design flood value of the target watershed according to the penalty likelihood function;
输出模块,用于输出所述预测的设计洪水值。An output module for outputting the predicted design flood value.
本发明实施例中,通过获取目标流域的年最大洪峰流量信息序列;依据所 述年最大洪峰流量信息序列,获取皮尔逊III型分布的似然函数;依据所述皮 尔逊III型分布的似然函数,获取惩罚似然函数;依据所述惩罚似然函数,预 测所述目标流域的设计洪水值并输出所述预测的设计洪水值。这样由于依据皮 尔逊III型分布的似然函数获取的惩罚似然函数预测设计洪水值,从而可以减 小预测设计洪水值的误差。In the embodiment of the present invention, the annual maximum flood peak flow information sequence of the target watershed is obtained; according to the annual maximum flood peak flow information sequence, the likelihood function of the Pearson III distribution is obtained; according to the likelihood of the Pearson III distribution function to obtain a penalized likelihood function; according to the penalized likelihood function, predict the design flood value of the target watershed and output the predicted design flood value. In this way, since the penalized likelihood function obtained by the likelihood function of the Pearson type III distribution is used to predict the design flood value, the error of predicting the design flood value can be reduced.
附图说明Description of drawings
图1是本发明实施例提供的一种设计洪水值预测方法的流程图;Fig. 1 is a flow chart of a design flood value prediction method provided by an embodiment of the present invention;
图2是不同系数值的惩罚函数变化图;Fig. 2 is the change graph of the penalty function of different coefficient values;
图3是本发明实施例提供的一种设计洪水值预测装置的结构。FIG. 3 is a structure of a designed flood value prediction device provided by an embodiment of the present invention.
具体实施方式Detailed ways
下面将结合本发明实施例中的附图,对本发明实施例中的技术方案进行清 楚、完整地描述,显然,所描述的实施例是本申请一部分实施例,而不是全部 的实施例。基于本申请中的实施例,本领域普通技术人员在没有作出创造性劳 动前提下所获得的所有其他实施例,都属于本申请保护的范围。The technical solutions in the embodiments of the present invention will be clearly and completely described below with reference to the accompanying drawings in the embodiments of the present invention. Obviously, the described embodiments are part of the embodiments of the present application, rather than all of the embodiments. Based on the embodiments in the present application, all other embodiments obtained by those of ordinary skill in the art without creative work shall fall within the protection scope of the present application.
本申请的说明书和权利要求书中的术语“第一”、“第二”等是用于区别类 似的对象,而不用于描述特定的顺序或先后次序。应该理解这样使用的数据在 适当情况下可以互换,以便本申请的实施例能够以除了在这里图示或描述的那 些以外的顺序实施,且“第一”、“第二”所区别的对象通常为一类,并不限定 对象的个数,例如第一对象可以是一个,也可以是多个。The terms "first", "second" and the like in the description and claims of the present application are used to distinguish similar objects, and are not used to describe a specific order or sequence. It is to be understood that the data so used are interchangeable under appropriate circumstances so that the embodiments of the present application can be practiced in sequences other than those illustrated or described herein, and "first", "second" distinguishes Usually it is a class, and the number of objects is not limited. For example, the first object may be one or multiple.
请参见图1,图1是本发明实施例提供的一种设计洪水值预测方法的流程 图,如图1所示,包括以下步骤:Please refer to FIG. 1. FIG. 1 is a flowchart of a design flood value prediction method provided by an embodiment of the present invention. As shown in FIG. 1, the following steps are included:
步骤101、获取目标流域的年最大洪峰流量信息序列。Step 101: Obtain the information sequence of the annual maximum flood peak flow of the target watershed.
步骤102、依据所述年最大洪峰流量信息序列,获取皮尔逊III型分布的 似然函数。Step 102: Obtain the likelihood function of the Pearson III distribution according to the maximum peak flow information sequence of the year.
上述皮尔逊III型分布为一条一端有限一端无限的不对称分布单峰的概率 分布曲线。在一致性假定下,基于矩法能得到分布的参数估计量,但矩法无法 应用在非一致性条件中。因此,在非一致性条件下,皮尔逊III型分布时被广 泛应用于水文分析技术领域。The above-mentioned Pearson type III distribution is a probability distribution curve of asymmetric distribution with one end being finite and one end being infinite. Under the assumption of consistency, the parameter estimates of the distribution can be obtained based on the method of moments, but the method of moments cannot be used in non-uniform conditions. Therefore, under non-uniform conditions, Pearson type III distribution is widely used in the field of hydrological analysis technology.
步骤103、依据所述皮尔逊III型分布的似然函数,获取惩罚似然函数。Step 103: Obtain a penalty likelihood function according to the likelihood function of the Pearson III distribution.
步骤104、依据所述惩罚似然函数,预测所述目标流域的设计洪水值。Step 104: Predict the design flood value of the target watershed according to the penalized likelihood function.
步骤105、输出所述预测的设计洪水值。Step 105: Output the predicted design flood value.
上述步骤输出的预测设计洪水值可以作为水利工程建设的重要参照数据, 例如,根据所预测的设计洪水值,检验防洪水工建筑物设计是否满足设计要求。The predicted design flood value output from the above steps can be used as important reference data for water conservancy project construction, for example, according to the predicted design flood value, it is checked whether the design of the flood control building meets the design requirements.
本发明实施例中,通过上述步骤可以实现依据皮尔逊III型分布的似然函 数获取惩罚似然函数预测设计洪水值,从而可以减小预测设计洪水值的误差。In the embodiment of the present invention, through the above steps, it is possible to obtain the penalized likelihood function to predict the design flood value according to the likelihood function of the Pearson type III distribution, so that the error of predicting the design flood value can be reduced.
作为一种可选的实施方式,获取目标流域的年最大洪峰流量信息序列,包 括:As an optional implementation, obtain the annual maximum flood peak flow information sequence of the target watershed, including:
在所述目标流域的实际测量的洪水序列中,选取洪水流量的年最大值构成 年最大洪峰流量信息序列。In the actual measured flood sequence of the target watershed, the annual maximum value of the flood flow is selected to constitute the annual maximum flood peak flow information sequence.
径流由大气降水形成的,并通过流域内不同路径进入河流、湖泊或海洋的 水流,习惯上也表示一定时段内通过河流某一断面的水量,即径流量。因此, 径流量是指单位时间内通过目标流域某一断面的水量,径流量是陆地上最重要 的水文要素之一。日径流就是径流量的单位时间为日,即每日通过目标流域某 一断面的总水量。影响径流量的主要因素是气候因素和下垫面因素,气候因素 包括降雨强度和蒸发,下垫面因素包括几何因素、自然地理位置因素和人类活 动因素。可见,因不同影响因素的存在,每日通过目标流域某一断面的总水量 是不同的。Runoff is formed by atmospheric precipitation and enters rivers, lakes or oceans through different paths in the watershed. It is also customary to represent the amount of water passing through a section of a river in a certain period of time, that is, runoff. Therefore, runoff refers to the amount of water passing through a certain section of the target watershed per unit time, and runoff is one of the most important hydrological elements on land. Daily runoff is the unit time of runoff in days, that is, the total amount of water passing through a certain section of the target watershed every day. The main factors affecting runoff are climatic factors and underlying surface factors. Climatic factors include rainfall intensity and evaporation, and underlying surface factors include geometric factors, natural geographical location factors and human activity factors. It can be seen that due to the existence of different influencing factors, the daily total water volume passing through a certain section of the target watershed is different.
汇总目标流域的实际测量的洪水信息,形成每一年的洪水数据集。在每一 年的洪水数据集中,选取每一年中洪水流量的最大值,构成年最大洪峰流量信 息序列。The actual measured flood information of the target watershed is aggregated to form a flood dataset for each year. In the flood data set of each year, the maximum value of the flood flow in each year is selected to form the information sequence of the maximum annual flood peak flow.
该实施方式中,由于选取每一年中洪水流量的最大值作为年最大洪峰流量 信息序列,可以提高所获取的年最大洪峰流量信息的准确性。In this embodiment, since the maximum value of the flood flow in each year is selected as the information sequence of the annual maximum flood peak flow, the accuracy of the obtained annual maximum flood peak flow information can be improved.
可选的,所述依据所述年最大洪峰流量信息序列,获取皮尔逊III型分布 的似然函数,包括:Optionally, according to the maximum flood peak flow information sequence of the year, obtain the likelihood function of Pearson III distribution, including:
依据所述年最大洪峰流量信息序列,通过如下计算获取皮尔逊III型分布 的概率密度函数:According to the maximum flood peak flow information sequence of the year, the probability density function of Pearson III distribution is obtained by the following calculation:
其中,f(xt)为概率密度函数,t为协变量,α(t)为形状参数,β(t)为尺度参 数,r(t)为位置参数,xt为年最大洪峰流量信息序列;Among them, f(x t ) is the probability density function, t is the covariate, α(t) is the shape parameter, β(t) is the scale parameter, r(t) is the location parameter, and x t is the annual maximum peak flow information sequence ;
依据所述概率密度函数,通过如下计算获取皮尔逊III型分布的似然函数:According to the probability density function, the likelihood function of the Pearson III distribution is obtained by the following calculation:
其中,L(α(t),β(t),r(t))为似然函数,f(xt)为概率密度函数,t为协变量,α(t)为形状参数,β(t)为尺度参数,r(t)为位置参数,xt为年最大洪峰流量信息序列。where L(α(t), β(t), r(t)) is the likelihood function, f(x t ) is the probability density function, t is the covariate, α(t) is the shape parameter, β(t) ) is the scale parameter, r(t) is the location parameter, and x t is the annual maximum flood peak flow information sequence.
上述皮尔逊III型分布的概率密度函数中,t为协变量,α(t)形状参数,β(t) 尺度参数及r(t)位置参数均表示为协变量t的函数。协变量一般表示为时间,根 据时间的变化,形状参数、尺度参数和位置参数也会处于变化的状态。由于年 最大洪峰流量信息序列属于年极大值序列,皮尔逊III型分布会呈现出正偏特 征,即对应β(t)>0,且xt-r(t)≥0。In the probability density function of the above Pearson III distribution, t is a covariate, α(t) shape parameter, β(t) scale parameter and r(t) position parameter are all expressed as functions of covariate t. Covariates are generally expressed as time. According to the change of time, the shape parameters, scale parameters and position parameters will also be in a state of change. Since the information sequence of the annual maximum flood peak flow belongs to the annual maximum value sequence, the Pearson III distribution will show a positive bias, that is, the corresponding β(t)>0, and x t -r(t)≥0.
上述皮尔逊III型分布的似然函数取得极大值的一组参数值即为皮尔逊III 型分布参数的极大似然估计结果。A set of parameter values where the likelihood function of the above-mentioned Pearson type III distribution obtains a maximum value is the maximum likelihood estimation result of the parameters of the Pearson type III distribution.
该实施方式中,由于皮尔逊III型分布的似然函数可确定的非一致性条件 下的函数参数估计结果,所得参数估计结果更符合实际情况,从而提高了设计 洪水值预测结果的可靠性。In this embodiment, because the likelihood function of the Pearson type III distribution can determine the function parameter estimation result under non-uniform conditions, the obtained parameter estimation result is more in line with the actual situation, thereby improving the reliability of the design flood value prediction result.
可选的,所述依据所述皮尔逊III型分布的似然函数,获取惩罚似然函数, 包括:Optionally, obtaining a penalty likelihood function according to the likelihood function of the Pearson III distribution, including:
通过如下计算获取惩罚函数;The penalty function is obtained by the following calculation;
其中,π(xt-r(t))为惩罚函数,t为协变量,r(t)为位置参数,xt为年最大洪 峰流量信息序列,a、c、B分别为惩罚函数中的系数;Among them, π(x t -r(t)) is the penalty function, t is the covariate, r(t) is the location parameter, x t is the information sequence of the annual maximum flood peak flow, and a, c, and B are respectively in the penalty function. coefficient;
依据所述皮尔逊III型分布的似然函数和所述惩罚函数,通过如下计算获 取惩罚似然函数:According to the likelihood function of the Pearson III distribution and the penalty function, the penalty likelihood function is obtained by the following calculation:
其中,PL(α(t),β(t),r(t))为惩罚似然函数,t为协变量,α(t)为形状参数,β(t)为尺度参数,r(t)为位置参数,f(xt)为概率密度函数,π(xt-r(t))为惩罚函数。Among them, PL(α(t), β(t), r(t)) is the penalized likelihood function, t is the covariate, α(t) is the shape parameter, β(t) is the scale parameter, and r(t) is the position parameter, f(x t ) is the probability density function, and π(x t -r(t)) is the penalty function.
上述惩罚函数中,惩罚函数中的系数a和c反应了惩罚函数在(xt-r(t))≈0时 的惩罚力度,B为惩罚函数的作用阈值,当xt-r(t)≤B时,惩罚函数将生效并限 制分布中位置参数的取值。In the above penalty function, the coefficients a and c in the penalty function reflect the penalty intensity of the penalty function when (x t -r(t))≈0, B is the action threshold of the penalty function, when x t -r(t) When ≤B, the penalty function will take effect and limit the value of the position parameter in the distribution.
将上述惩罚函数和皮尔逊III型分布的似然函数进行组合相乘,获取上述 惩罚似然函数。The above penalty function is combined and multiplied by the likelihood function of the Pearson III distribution to obtain the above penalty likelihood function.
上述惩罚函数π(xt-r(t))的取值范围介于0~1之间,当xt-r(t)>B时,有 π(xt-r(t))=1,此时惩罚似然函数与上述皮尔逊III型分布的似然函数完全相同。 当xt-r(t)≤B时,惩罚函数π(xt-r(t))介于0~1之间,从而减少了惩罚似然函数的 取值。The value range of the above penalty function π(x t -r(t)) is between 0 and 1. When x t -r(t)>B, there is π(x t -r(t))=1 , the penalty likelihood function is exactly the same as the likelihood function of the Pearson III distribution above. When x t -r(t)≤B, the penalty function π(x t -r(t)) is between 0 and 1, thereby reducing the value of the penalty likelihood function.
请参见图2,图2为不同系数值的惩罚函数变化图,如图2所示,图2反 映了惩罚函数中的系数a和c取不同值时,惩罚函数的在xt-r(t)∈[0,0.05]区间上的 变化情况。可以看出,a和c的取值越大,惩罚函数对(xt-r(t))≈0时的惩罚力度 越大,即(xt-r(t))≈0的可能性越小。一般而言,a和c取值推荐a>50,c为大于等 于1的奇数。Please refer to Figure 2. Figure 2 is a graph of the change of the penalty function with different coefficient values. As shown in Figure 2, Figure 2 reflects that when the coefficients a and c in the penalty function take different values, the change of the penalty function in x t -r(t ) ∈ [0,0.05] on the interval. It can be seen that the larger the values of a and c are, the greater the penalty function is for (x t -r(t))≈0, that is, the more likely it is that (x t -r(t))≈0 Small. Generally speaking, the values of a and c are recommended as a>50, and c is an odd number greater than or equal to 1.
采用极大似然法求得最优参数估计的原理是通过皮尔逊III型分布的似然 函数取最大值的参数作为最优参数估计结果,因此,在似然函数中引入惩罚函 数可使得xt-r(t)落入区间[0,B]之间的概率减少。为避免出现(xt-r(t))≈0这一情况, 惩罚函数的作用阈值B的取值不宜过大,通常取B∈[0.03,0.1]。The principle of using the maximum likelihood method to obtain the optimal parameter estimation is to take the parameter with the maximum value from the likelihood function of the Pearson III distribution as the optimal parameter estimation result. Therefore, the introduction of a penalty function into the likelihood function can make x The probability of t - r(t) falling between the interval [0,B] decreases. In order to avoid the situation of (x t -r(t))≈0, the value of the action threshold B of the penalty function should not be too large, usually B∈[0.03,0.1].
因此,惩罚函数中的系数可取a=100,B=0.05,c=3,在此情景下,当 xt-r(t)∈[0,0.03]时,有π(xt-r(t))≈0,此时惩罚似然函数PL(α(t),β(t),r(t))≈0,从而避 免采用极大似然法进行参数寻优时出现(xt-r(t))≈0的情况。Therefore, the coefficients in the penalty function can take a=100, B=0.05, and c=3. In this case, when x t -r(t)∈[0,0.03], there is π(x t -r(t ))≈0, at this time the penalized likelihood function PL(α(t),β(t),r(t))≈0, so as to avoid the occurrence of (x t -r (t)) ≈ 0 case.
该实施方式中,由于依据皮尔逊III型分布的似然函数,获取惩罚似然函 数,从而可以提高最优参数的准确性。In this embodiment, since the penalized likelihood function is obtained according to the likelihood function of the Pearson type III distribution, the accuracy of the optimal parameter can be improved.
可选的,所述依据所述惩罚似然函数,预测所述目标流域的设计洪水值, 包括:Optionally, predicting the design flood value of the target watershed according to the penalty likelihood function, including:
依据所述惩罚似然函数,获取惩罚似然函数极大值对应的惩罚似然函数估 计参数;According to the penalty likelihood function, obtain the penalty likelihood function estimation parameter corresponding to the maximum value of the penalty likelihood function;
依据所述惩罚似然函数估计参数,通过如下计算设计洪水值:According to the estimated parameters of the penalized likelihood function, the design flood value is calculated as follows:
其中,Qp为设计洪水值,gaminv表示gamma分布累积分布函数的反函数, p为超越概率,t为协变量,β(t)为惩罚似然函数估计尺度参数,r(t)为惩罚似 然函数估计位置参数。Among them, Q p is the design flood value, gaminv is the inverse function of the cumulative distribution function of the gamma distribution, p is the transcendence probability, t is the covariate, β(t) is the estimated scale parameter of the penalized likelihood function, and r(t) is the penalized likelihood function. Then the function estimates the position parameter.
基于极大似然原理,当惩罚似然函数取极大值时,其所对应的参数就是惩 罚似然函数估计参数,进一步的,根据惩罚似然函数估计参数,获取在超越概 率p下年最大洪峰流量信息序列对应的预测设计洪水值。极大似然原理指在参 数的可能取值范围内,选取使函数达到最大的参数值,作为参数的估计值。Based on the principle of maximum likelihood, when the penalized likelihood function takes a maximum value, the corresponding parameter is the estimated parameter of the penalized likelihood function. Further, the parameter is estimated according to the penalized likelihood function to obtain the maximum value in the next year under the transcendence probability p. The predicted design flood value corresponding to the flood peak flow information sequence. The maximum likelihood principle refers to selecting the parameter value that maximizes the function within the possible value range of the parameter as the estimated value of the parameter.
可采用信息评价准则来验证分布模型的优劣,常用的主要有赤池信息量准 则(AIC)和贝叶斯信息准则(BIC),当存在多组分布模型进行必选时,AIC/BIC 值最小的那一组模型即为最优模型:The information evaluation criterion can be used to verify the pros and cons of the distribution model. The commonly used ones are the Akaike Information Criterion (AIC) and the Bayesian Information Criterion (BIC). When there are multiple groups of distribution models, the AIC/BIC value is the smallest. The set of models is the optimal model:
AIC=-2LLF+2numParAIC=-2LLF+2numPar
BIC=-2LLF+numPar×log(n)BIC=-2LLF+numPar×log(n)
式中,LLF为最大对数似然估计函数值,例如,在惩罚似然函数中,LLF表 示为惩罚似然函数的极大值取对数的数值,n为年最大洪峰流量信息序列的长 度,numPar为分布中待估计参数数量,对于一致性条件下的皮尔逊III型分布, 当非一致性皮尔逊III型分布的尺度和形状参数为固定值,位置参数表示为时 间t的线性函数时,即r(t)=at+b,则numPar=4。对于有着显著变化趋势的洪水序 列,可分别采用一致性条件下的皮尔逊III型分布、基于惩罚似然函数的非一 致性皮尔逊III型分布对年最大洪峰流量信息序列进行拟合,基于AIC/BIC检 验结果或其他模型诊断方法,验证惩罚似然函数在理论上的合理性和可行性。In the formula, LLF is the maximum log-likelihood estimation function value. For example, in the penalized likelihood function, LLF is expressed as the logarithm of the maximum value of the penalized likelihood function, and n is the length of the annual maximum flood peak flow information sequence. , numPar is the number of parameters to be estimated in the distribution. For the Pearson III distribution under the consistency condition, when the scale and shape parameters of the non-consistent Pearson III distribution are fixed values, and the position parameter is expressed as a linear function of time t , that is, r(t)=at+b, then numPar=4. For flood sequences with significant change trends, the Pearson III distribution under consistent conditions and the non-consistent Pearson III distribution based on penalized likelihood function can be used to fit the information sequence of the annual maximum flood peak flow. Based on AIC /BIC test results or other model diagnostic methods to verify the theoretical rationality and feasibility of the penalized likelihood function.
该实施方式中,由于将惩罚似然函数极大值对应的参数作为惩罚似然函数 估计参数,从而可以提高洪水预测值的准确性。In this embodiment, since the parameter corresponding to the maximum value of the penalized likelihood function is used as the estimated parameter of the penalized likelihood function, the accuracy of the flood prediction value can be improved.
请参见图3,图3是本发明实施例提供的一种设计洪水值预测装置的结构 图,如图3所示,设计洪水值预测装置包括:Please refer to Fig. 3. Fig. 3 is a structural diagram of a design flood value prediction device provided by an embodiment of the present invention. As shown in Fig. 3, the design flood value prediction device includes:
第一获取模块301,用于获取目标流域的年最大洪峰流量信息序列;The first obtaining
第二获取模块302,用于依据所述年最大洪峰流量信息序列,获取皮尔逊 III型分布的似然函数;The second obtaining
第三获取模块303,用于依据所述皮尔逊III型分布的似然函数,获取惩 罚似然函数;The
第四获取模块304,用于依据所述惩罚似然函数,预测所述目标流域的设 计洪水值;The
输出模块305,用于输出所述预测的设计洪水值。The
可选的,第一获取模块用于在所述目标流域的实际测量的洪水序列中,选 取洪水流量的年最大值构成年最大洪峰流量信息序列。Optionally, the first acquisition module is configured to select the annual maximum value of the flood flow from the actually measured flood sequence of the target watershed to form the annual maximum flood peak flow information sequence.
可选的,第二获取模块用于依据所述年最大洪峰流量信息序列,通过如下 计算获取皮尔逊III型分布的概率密度函数:Optionally, the second acquisition module is used to obtain the probability density function of Pearson type III distribution according to the maximum flood peak flow information sequence of the year, by the following calculation:
其中,f(xt)为概率密度函数,t为协变量,α(t)为形状参数,β(t)为尺度参 数,r(t)为位置参数,xt为年最大洪峰流量信息序列;Among them, f(x t ) is the probability density function, t is the covariate, α(t) is the shape parameter, β(t) is the scale parameter, r(t) is the location parameter, and x t is the annual maximum peak flow information sequence ;
依据所述概率密度函数,通过如下计算获取皮尔逊III型分布的似然函数:According to the probability density function, the likelihood function of the Pearson III distribution is obtained by the following calculation:
其中,L(α(t),β(t),r(t))为似然函数,f(xt)为概率密度函数,t为协变量,α(t)为形状参数,β(t)为尺度参数,r(t)为位置参数,xt为年最大洪峰流量信息序列。where L(α(t), β(t), r(t)) is the likelihood function, f(x t ) is the probability density function, t is the covariate, α(t) is the shape parameter, β(t) ) is the scale parameter, r(t) is the location parameter, and x t is the annual maximum flood peak flow information sequence.
可选的,第三获取模块用于通过如下计算获取惩罚函数;Optionally, the third obtaining module is used to obtain the penalty function through the following calculation;
其中,π(xt-r(t))为惩罚函数,t为协变量,r(t)为位置参数,xt为年最大洪 峰流量信息序列,a、c、B分别为惩罚函数中的系数;Among them, π(x t -r(t)) is the penalty function, t is the covariate, r(t) is the location parameter, x t is the information sequence of the annual maximum flood peak flow, and a, c, and B are respectively in the penalty function. coefficient;
依据所述皮尔逊III型分布的似然函数和所述惩罚函数,通过如下计算获 取惩罚似然函数:According to the likelihood function of the Pearson III distribution and the penalty function, the penalty likelihood function is obtained by the following calculation:
其中,PL(α(t),β(t),r(t))为惩罚似然函数,t为协变量,α(t)为形状参数,β(t)为尺度参数,r(t)为位置参数,f(xt)为概率密度函数,π(xt-r(t))为惩罚函数。Among them, PL(α(t), β(t), r(t)) is the penalized likelihood function, t is the covariate, α(t) is the shape parameter, β(t) is the scale parameter, and r(t) is the position parameter, f(x t ) is the probability density function, and π(x t -r(t)) is the penalty function.
可选的,第四获取模块用于依据所述惩罚似然函数,获取惩罚似然函数极 大值对应的惩罚似然函数估计参数;Optionally, the fourth acquisition module is used to obtain the penalty likelihood function estimation parameter corresponding to the penalty likelihood function maximum value according to the penalty likelihood function;
依据所述惩罚似然函数估计参数,通过如下计算设计洪水值:According to the estimated parameters of the penalized likelihood function, the design flood value is calculated as follows:
其中,Qp为设计洪水值,gaminv表示gamma累积分布函数的反函数,p为 超越概率,t为协变量,β(t)为惩罚似然函数估计尺度参数,r(t)为惩罚似然函 数估计位置参数。Among them, Q p is the design flood value, gaminv is the inverse function of the gamma cumulative distribution function, p is the transcendence probability, t is the covariate, β(t) is the estimated scale parameter of the penalized likelihood function, and r(t) is the penalized likelihood The function estimates positional parameters.
本发明实施例提供的设计洪水值预测装置能够实现图1的方法实施例中 的各个过程,为避免重复,这里不再赘述。The designed flood value prediction device provided in the embodiment of the present invention can implement each process in the method embodiment of FIG. 1 , and in order to avoid repetition, details are not repeated here.
需要说明的是,本发明实施例中的设计洪水值预测装置可以是装置,也可 以是电子设备中的部件、集成电路、或芯片。It should be noted that, the device for predicting the design flood value in the embodiment of the present invention may be a device, and may also be a component, an integrated circuit, or a chip in an electronic device.
需要说明的是,在本文中,术语“包括”、“包含”或者其任何其他变体意 在涵盖非排他性的包含,从而使得包括一系列要素的过程、方法、物品或者装 置不仅包括那些要素,而且还包括没有明确列出的其他要素,或者是还包括为 这种过程、方法、物品或者装置所固有的要素。在没有更多限制的情况下,由 语句“包括一个……”限定的要素,并不排除在包括该要素的过程、方法、物 品或者装置中还存在另外的相同要素。此外,需要指出的是,本申请实施方式 中的方法和装置的范围不限按示出或讨论的顺序来执行功能,还可包括根据所 涉及的功能按基本同时的方式或按相反的顺序来执行功能,例如,可以按不同 于所描述的次序来执行所描述的方法,并且还可以添加、省去、或组合各种步 骤。另外,参照某些示例所描述的特征可在其他示例中被组合。It should be noted that, herein, the terms "comprising", "comprising" or any other variation thereof are intended to encompass non-exclusive inclusion, such that a process, method, article or device comprising a series of elements includes not only those elements, It also includes other elements not expressly listed or inherent to such a process, method, article or apparatus. Without further limitation, an element qualified by the phrase "comprising a..." does not preclude the presence of additional identical elements in a process, method, article or apparatus that includes the element. Furthermore, it should be noted that the scope of the methods and apparatus in the embodiments of the present application is not limited to performing the functions in the order shown or discussed, but may also include performing the functions in a substantially simultaneous manner or in the reverse order depending on the functions involved. To perform functions, for example, the described methods may be performed in an order different from that described, and various steps may also be added, omitted, or combined. Additionally, features described with reference to some examples may be combined in other examples.
通过以上的实施方式的描述,本领域的技术人员可以清楚地了解到上述实 施例方法可借助软件加必需的通用硬件平台的方式来实现,当然也可以通过硬 件,但很多情况下前者是更佳的实施方式。基于这样的理解,本申请的技术方 案本质上或者说对现有技术做出贡献的部分可以以软件产品的形式体现出来, 该计算机软件产品存储在一个存储介质(如ROM/RAM、磁碟、光盘)中,包 括若干指令用以使得一台终端(可以是手机,计算机,服务器,空调器,或者 网络设备等)执行本申请各个实施例所述的方法。From the description of the above embodiments, those skilled in the art can clearly understand that the method of the above embodiment can be implemented by means of software plus a necessary general hardware platform, and of course can also be implemented by hardware, but in many cases the former is better implementation. Based on this understanding, the technical solutions of the present application can be embodied in the form of software products in essence or the parts that make contributions to the prior art, and the computer software products are stored in a storage medium (such as ROM/RAM, magnetic disk, CD-ROM), including several instructions to make a terminal (which may be a mobile phone, a computer, a server, an air conditioner, or a network device, etc.) execute the methods described in the various embodiments of this application.
上面结合附图对本申请的实施例进行了描述,但是本申请并不局限于上述 的具体实施方式,上述的具体实施方式仅仅是示意性的,而不是限制性的,本 领域的普通技术人员在本申请的启示下,在不脱离本申请宗旨和权利要求所保 护的范围情况下,还可做出很多形式,均属于本申请的保护之内。The embodiments of the present application have been described above in conjunction with the accompanying drawings, but the present application is not limited to the above-mentioned specific embodiments, which are merely illustrative rather than restrictive. Under the inspiration of this application, without departing from the scope of protection of the purpose of this application and the claims, many forms can be made, which all fall within the protection of this application.
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Citations (7)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN104615845A (en) * | 2014-12-19 | 2015-05-13 | 兰州大学 | Supercritical flood risk analysis method |
KR20170005553A (en) * | 2015-07-06 | 2017-01-16 | 주식회사 유일기연 | Floods, drought assessment and forecasting techniques development for intelligent service |
CN106446547A (en) * | 2016-09-27 | 2017-02-22 | 华中科技大学 | Generalized second-category beta distribution based flood frequency analysis method |
CN107832935A (en) * | 2017-10-30 | 2018-03-23 | 中国水利水电科学研究院 | Method and device for determining design value of hydrological variable |
CN109284477A (en) * | 2018-09-29 | 2019-01-29 | 中国水利水电科学研究院 | A method and device for probabilistic calculation of combination of abundance and dryness of hydrological sequence |
CN110135114A (en) * | 2019-06-06 | 2019-08-16 | 中国水利水电科学研究院 | Method and device for determining minimum navigable water level of river design |
CN111241478A (en) * | 2020-01-08 | 2020-06-05 | 南京大学 | Flood frequency estimation method considering historical flood |
-
2020
- 2020-09-17 CN CN202010978962.XA patent/CN112149893A/en active Pending
Patent Citations (7)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN104615845A (en) * | 2014-12-19 | 2015-05-13 | 兰州大学 | Supercritical flood risk analysis method |
KR20170005553A (en) * | 2015-07-06 | 2017-01-16 | 주식회사 유일기연 | Floods, drought assessment and forecasting techniques development for intelligent service |
CN106446547A (en) * | 2016-09-27 | 2017-02-22 | 华中科技大学 | Generalized second-category beta distribution based flood frequency analysis method |
CN107832935A (en) * | 2017-10-30 | 2018-03-23 | 中国水利水电科学研究院 | Method and device for determining design value of hydrological variable |
CN109284477A (en) * | 2018-09-29 | 2019-01-29 | 中国水利水电科学研究院 | A method and device for probabilistic calculation of combination of abundance and dryness of hydrological sequence |
CN110135114A (en) * | 2019-06-06 | 2019-08-16 | 中国水利水电科学研究院 | Method and device for determining minimum navigable water level of river design |
CN111241478A (en) * | 2020-01-08 | 2020-06-05 | 南京大学 | Flood frequency estimation method considering historical flood |
Non-Patent Citations (1)
Title |
---|
SONG XINYI ET AL: ""Penalized maximum likelihood estimators for the nonstationary Pearson type 3 distribution"", 《JOURNAL OF HYDROLOGY》, pages 580 - 582 * |
Cited By (1)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN117827935A (en) * | 2024-01-08 | 2024-04-05 | 湖南五凌电力科技有限公司 | A method for predicting flood inundation risk |
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