论文标题
欧洲极端寒冷和微弱事件的高斯副群体模型以冬季天气制度为条件
Gaussian copula modeling of extreme cold and weak-wind events over Europe conditioned on winter weather regimes
论文作者
论文摘要
需要向可再生能源过渡以减轻气候变化。在欧洲,这种过渡是由风能领导的,这是增长最快的能源之一。但是,能源需求和生产对气象条件和多个时间尺度下的大气变异性很敏感。为了在这两个变量之间达到所需的平衡,必须在能源系统的设计中考虑高需求和低风能供应的关键条件。我们描述了一种模拟气象变量联合分布的方法,而无需对其边际分布做出任何假设。在这种情况下,高斯库拉斯用于模拟冷和弱事件的相关性质。边缘分布以逻辑回归为模型,将两组二进制变量定义为预测因素:四个大规模的天气制度和延长的冬季几个月。通过将此框架应用于ERA5数据,我们可以计算高分辨率网格(0.25 ver)上冷和虚弱事件共同出现的关节概率。我们的结果表明,a)在建模寒冷和弱的事件时必须考虑天气方案,b)必须考虑到这些事件建模时这些事件之间的相关性,c)我们需要分别分析这些事件,c)我们需要分别分析这些事件,d)与复合事件的估计数量最高的天数与北大西洋振荡的平均和卢思堡(Finland and Lithemia)的平均阶段相关联(3天) 2月)和斯堪的纳维亚的阻塞模式(1月份的爱尔兰平均3天和2月的丹麦)。此信息可能与此类事件的季节性预测相关的申请。
A transition to renewable energy is needed to mitigate climate change. In Europe, this transition has been led by wind energy, which is one of the fastest growing energy sources. However, energy demand and production are sensitive to meteorological conditions and atmospheric variability at multiple time scales. To accomplish the required balance between these two variables, critical conditions of high demand and low wind energy supply must be considered in the design of energy systems. We describe a methodology for modeling joint distributions of meteorological variables without making any assumptions about their marginal distributions. In this context, Gaussian copulas are used to model the correlated nature of cold and weak-wind events. The marginal distributions are modeled with logistic regressions defining two sets of binary variables as predictors: four large-scale weather regimes and the months of the extended winter season. By applying this framework to ERA5 data, we can compute the joint probabilities of co-occurrence of cold and weak-wind events on a high-resolution grid (0.25 deg). Our results show that a) weather regimes must be considered when modeling cold and weak-wind events, b) it is essential to account for the correlations between these events when modeling their joint distribution, c) we need to analyze each month separately, and d) the highest estimated number of days with compound events are associated with the negative phase of the North Atlantic Oscillation (3 days on average over Finland, Ireland, and Lithuania in January, and France and Luxembourg in February) and the Scandinavian Blocking pattern (3 days on average over Ireland in January and Denmark in February). This information could be relevant for application in sub-seasonal to seasonal forecasts of such events.