What could we have learnt from the previous flood data to predict losses caused by the 1980, 1986, and 1998 catastrophic floods in Ukrainian Transcarpathian?

D. Stefanyshyn
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引用次数: 1

Abstract

This paper explores some aspects relating to retrospective predicting the confirmed monetary losses caused by the disastrous floods of 1980, 1986, and 1998 in the Tisza River basin within the Transcarpathian region of Ukraine. The research was based on two time series – the losses because of past floods and the maxima water discharges gauged at the hydrological station near the village of Vylok, Vynohradiv district. The main aim of the research was to make out whether it had been the possibility to predict the losses due to those floods in advance.In solving the task, there was revealed and modelled the dependence of the risk of losses due to the floods in Transcarpathia on the maximum water discharges of the Tisza River gauged at the “Vylok” hydrological station. Predicting was based on the hypothesis of the stationary random process for maximum water discharges, which allowed using an empirical distribution function of a random variable regarding flood water discharges assessing the risk of flood losses.Retrospective predicting of the losses caused by the floods of 1980, 1986, and 1998 was carried out by means of a combined situational-inductive predictive modelling method (CSIPMM), being an original author’s development. The method relates to predicting the behaviour of complex dynamic systems based on monitoring findings presented as time series data reflecting evolutions of a resulting (dependent) variable and an explaining (independent) variable (predictor). The method uses extrapolation-regression type models. According to this method, the prediction task is performed in two stages. The first stage realises the retrospective situational modelling task aiming to obtain a set of simple regressions (situational models) built on data of sample time series. The situational models are accepted to be adequate or relevant ones only within certain periods of time determined as situations. In the second stage, based on the generalization (on an ensemble) of the obtained retrospective situational models, inductive “levels” models are built, which reflect the behaviour of a controlled parameter of the system or process (a resulting variable) at several fixed values of a predictor in time. The inductive models are used in extrapolative predicting situational models belonging to future periods (situations).In total, three predictions were made: (1) taking into account the annual maximum flood discharges from 1954 to 1979 (before the flood of 1980); (2) the same from 1954 to 1985 (before the flood of 1986); (3) the same from 1954 to 1997 (before the flood of 1998). The study found that there had been a possibility to predict the confirmed monetary losses inflicted by the flood of 1986 and 1998 (relative predicting errors of 7.2-8.7% and 6.0-12.8% depending on the prediction options).
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我们可以从以前的洪水数据中学到什么来预测1980年、1986年和1998年乌克兰喀尔巴阡山脉的灾难性洪水造成的损失?
本文探讨了回溯预测1980年、1986年和1998年乌克兰外喀尔巴阡地区Tisza河流域已确认的灾难性洪水造成的经济损失的一些方面。这项研究基于两个时间序列——过去洪水造成的损失和Vynohradiv地区Vylok村附近水文站测量的最大水量。这项研究的主要目的是确定是否有可能提前预测洪水造成的损失。在解决这个问题的过程中,揭示并模拟了由“Vylok”水文站测量的Tisza河最大水量与外喀尔巴阡洪水造成的损失风险的依赖关系。预测是基于最大水量的平稳随机过程假设,这允许使用关于洪水水量的随机变量的经验分布函数来评估洪水损失的风险。采用情景-归纳相结合的预测建模方法(CSIPMM)对1980年、1986年和1998年三次洪涝灾害的损失进行了回顾性预测,是笔者的独创。该方法是基于监测结果来预测复杂动态系统的行为,这些结果以时间序列数据的形式呈现,反映了结果(因变量)和解释(独立)变量(预测器)的演变。该方法采用外推回归型模型。根据该方法,预测任务分两个阶段进行。第一阶段实现回顾性情景建模任务,旨在获得一组基于样本时间序列数据的简单回归(情景模型)。情境模型只有在确定为情境的特定时期内才被认为是适当的或相关的。在第二阶段,基于所获得的回顾性情景模型的泛化(基于集成),建立归纳“水平”模型,该模型反映了系统或过程的受控参数(结果变量)在时间预测器的几个固定值上的行为。归纳模型用于外推预测属于未来时期(情景)的情景模型。结果表明:(1)考虑了1954 ~ 1979年(1980年洪涝之前)的年最大洪流量;(2) 1954 ~ 1985年(1986年洪涝前)基本相同;(3) 1954 ~ 1997年(1998年洪水前)基本相同。研究发现,已经有可能预测1986年和1998年洪水造成的确认的经济损失(根据预测选项的不同,相对预测误差为7.2-8.7%和6.0-12.8%)。
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