The Peace-Athabasca Delta (PAD) of northwestern Alberta is one of the largest inland freshwater deltas in the world, laying at the confluence of the Peace and Athabasca Rivers. The PAD is recognized as a having unique ecological significance and periodic ice jam flooding from both rivers is an important feature of its current ecology. Past studies have debated whether a change in ice jam flood (IJF) frequency on the Peace River has recently occurred, and what factors might be driving any perceived changes. This study contributes to this debate by addressing two questions: (1) what factors are most predictive of Peace River IJFs, and (2) how might climate change impact IJF frequency? This work starts with a physically-based conceptual model of the necessary conditions for a large Peace River IJF, and the factors that indicate whether those conditions are met. Logistic regression is applied to the historical flood record to determine which combination of hydroclimatic and riverine factors best predict IJFs and the uncertainty in those relationships given the available data. Winter precipitation and temperature are most predictive of Peace River IJFs, while freeze-up elevation contains little predictive power and is not closely related to IJF occurrence. The best logistic regression model is forced with downscaled climate change scenarios from multiple climate models to project IJF frequency for a variety of plausible futures. Parametric uncertainty in the best logistic regression model is propagated into the projections using a parametric bootstrap to sample many plausible statistical models. Although there is variability across emissions scenarios and climate models, all projections indicate that the frequency of Peace River IJFs is likely to decrease substantially in the coming decades, and that average waiting times between future IJFs will likely surpass recent experience.
翻译:艾伯塔西北省和平-阿萨巴斯卡三角洲(PAD)是全世界最大的内陆淡水三角洲之一,位于和平河和阿塔帕斯卡河汇合处。人们公认PAD是一个独特的生态意义,两河定期的冰封洪水是其当前生态的一个重要特征。过去的研究辩论了和平河冰封洪水频率最近是否发生变化,以及哪些因素可能导致任何已知的变化。本研究解决了两个问题,为本次辩论提供了两个问题:(1)和平河IJF的预测力最高,以及(2)气候变化对IJF的预测力可能有多大影响?这项工作始于对大和平河IJF必要条件的物理概念模型,以及表明这些条件是否得到满足的各种因素。对历史洪水记录适用了退缩法,以确定哪些是水文和河流因素的组合,哪些是预示着IJF的排放量模型,以及根据现有数据,哪些是和平河IJF的预测力流和温度最能预测力的预测力变化率最高,同时,在F的不断冻结的精确度中,一个最精确的时期,可能与I的I的精确度预测力与I的精确度模型有关。