论文标题
建模季节性差异对降雨最大差异的影响
Implications of Modeling Seasonal Differences in the Extremal Dependence of Rainfall Maxima
论文作者
论文摘要
为了对极端降雨进行建模,广泛使用的棕色最大稳定模型扩展了变量图的概念以适合Bloc Maxima,从而可以对空间数据显示的极端依赖性进行明确的建模。这种极端依赖性源于观察到的降雨的几何特征,这与不同的气象过程有关,通常在设计研究模型时被认为是恒定的。但是,根据该地区的不同,随着促进降雨产生过程随着季节而变化的主要气象条件,这种依赖性可能会在全年中发生变化。因此,这项研究分析了极端依赖性季节变化对柏林 - 布兰登堡地区年度最大最大值建模的影响。在这项研究中,两个季节被认为是不同主导气象条件的代理:夏季,用于降雨和冬季/层状降雨的冬季。使用两个季节的最大值,我们将线性模型的技能与空间协变量(假定空间独立性)与棕色最大最大稳定模型的技能进行了比较。这种比较显示季节之间有很大的差异,各向同性棕色刺激模型显示出冬季最大值的技能丧失。我们得出的结论是,使用Brown-Resnick模型时通常做出的假设适用于夏季建模(即对流)事件,但应采取进一步的工作以建模其他类型的降水制度。
For modeling extreme rainfall, the widely used Brown-Resnick max-stable model extends the concept of the variogram to suit bloc maxima, allowing the explicit modeling of the extremal dependence shown by the spatial data. This extremal dependence stems from the geometrical characteristics of the observed rainfall, which is associated with different meteorological processes and is usually considered to be constant when designing the model for a study. However, depending on the region, this dependence can change throughout the year, as the prevailing meteorological conditions that drive the rainfall generation process change with the season. Therefore, this study analyzes the impact of the seasonal change in extremal dependence for the modeling of annual block maxima in the Berlin-Brandenburg region. For this study, two seasons were considered as proxies for different dominant meteorological conditions: summer for convective rainfall and winter for frontal/stratiform rainfall. Using maxima from both seasons, we compared the skill of a linear model with spatial covariates (that assumed spatial independence) with the skill of a Brown-Resnick max-stable model. This comparison showed a considerable difference between seasons, with the isotropic Brown-Resnick model showing considerable loss of skill for the winter maxima. We conclude that the assumptions commonly made when using the Brown-Resnick model are appropriate for modeling summer (i.e., convective) events, but further work should be done for modeling other types of precipitation regimes.