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EVALUATION OF ICE THICKNESS AS A PARAMETER IN RIVERBREAK-UP FORECAST MODELLING

机译:以冰厚度作为参数进行河道预报预测的评估

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During spring break-up, the Athabasca River frequently experiences ice jams in the vicinityof the City of Fort McMurray. Because of the danger to life and property associated with ice jam relatedflooding, a method of forecasting the risk of a severe break-up would be highly beneficial. While icethickness has been identified decades ago as a key factor in forecasting river ice break-up, it is onlyrecently that any serious scientific effort has been made to include it in a quantitative ice jam forecastmodel. Both recent forecast models, a linear multiple regression model and a fuzzy expert system, for theAthabasca River are very sensitive to the measured value of ice thickness. This paper presents theresults of an extensive investigation into the ice thickness measurements as part of establishing acomplete database from which to develop future models. The effect of this research on the previouslydiscussed models is evaluated.
机译:在春天分手期间,Athabasca河经常在附近体验冰喀 麦克米堡市。由于与冰堵塞相关的生命和财产的危险 洪水,预测严重分手的风险的方法将是非常有益的。冰上 几十年前已经确定了厚度,作为预测河冰分手的关键因素,它只是 最近,已经在定量冰堵塞预测中将任何严肃的科学努力纳入其中 模型。最近的预测模型,线性多元回归模型和模糊专家系统,适用于 Athabasca河对冰厚度的测量值非常敏感。本文呈现 作为建立A的一部分的冰厚度测量的广泛调查结果 完整的数据库,从中开发未来的模型。这项研究对先前的影响 讨论的模型进行了评估。

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