arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 2003.05854stat.AP
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最大稳定过程与实况预报耦合的强降水空间模拟

Spatial Modeling of Heavy Precipitation by Coupling Weather Station Recordings and Ensemble Forecasts with Max-Stable Processes

Marco Oesting, Philippe Naveau

摘要:

由于物理现象的复杂性,暴雨事件的空间分布很难模拟。基于物理的数值模式通常可以提供物理上连贯的空间模式,但可能会错过一些重要的降水特征,如暴雨强度。然而,地面气象站的测量提供了足够的降雨强度,但大多数国家的天气记录网络往往在空间上过于稀疏,无法充分捕捉降雨模式。为了充分利用这两种信息来源,气候学家和水文学家一直在寻找能够有效合并不同类型降雨数据的模型。一个固有的困难是捕捉适当的多变量之间的降雨最大值的依赖结构。为此,多元极值理论建议使用最大稳定过程。这样的过程可以表示为一个隐藏的随机过程的独立副本的最大线性组合加权的泊松点过程。在实践中,这个隐藏过程的选择是不平凡的,特别是如果各向异性,非平稳性和块金效应存在于手头的空间数据。通过耦合预报集合数据从法国国家气象局(Météo-France)与当地的观测,我们构建和比较不同类型的数据驱动的最大稳定的过程,是简约的参数,易于模拟和能够再现块金效应和空间非平稳性。我们还比较了我们的新方法与经典的空间极值理论,如布朗-雷斯尼克过程的方法。

英文摘要:

Due to complex physical phenomena, the distribution of heavy rainfall events is difficult to model spatially. Physically based numerical models can often provide physically coherent spatial patterns, but may miss some important precipitation features like heavy rainfall intensities. Measurements at ground-based weather stations, however, supply adequate rainfall intensities, but most national weather recording networks are often spatially too sparse to capture rainfall patterns adequately. To bring the best out of these two sources of information, climatologists and hydrologists have been seeking models that can efficiently merge different types of rainfall data. One inherent difficulty is to capture the appropriate multivariate dependence structure among rainfall maxima. For this purpose, multivariate extreme value theory suggests the use of a max-stable process. Such a process can be represented by a max-linear combination of independent copies of a hidden stochastic process weighted by a Poisson point process. In practice, the choice of this hidden process is non-trivial, especially if anisotropy, non-stationarity and nugget effects are present in the spatial data at hand. By coupling forecast ensemble data from the French national weather service (Météo-France) with local observations, we construct and compare different types of data driven max-stable processes that are parsimonious in parameters, easy to simulate and capable of reproducing nugget effects and spatial non-stationarities. We also compare our new method with classical approaches from spatial extreme value theory such as Brown-Resnick processes.

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