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An adaptive two-stage analog/regression model for probabilistic prediction of small-scale precipitation in France

机译:法国小规模降水概率预测的自适应两阶段模拟/回归模型

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Statistical downscaling models (SDMs) are often used to produce local weather scenarios from large-scale atmospheric information. SDMs include transfer functions which are based on a?statistical link identified from observations between local weather and a?set of large-scale predictors. As physical processes driving surface weather vary in time, the most relevant predictors and the regression link are likely to vary in time too. This is well known for precipitation for instance and the link is thus often estimated after some seasonal stratification of the data. In this study, we present a?two-stage analog/regression model where the regression link is estimated from atmospheric analogs of the current prediction day. Atmospheric analogs are identified from fields of geopotential heights at 1000 and 500?hPa. For the regression stage, two generalized linear models are further used to model the probability of precipitation occurrence and the distribution of non-zero precipitation amounts, respectively. The two-stage model is evaluated for the probabilistic prediction of small-scale precipitation over France. It noticeably improves the skill of the prediction for both precipitation occurrence and amount. As the analog days vary from one prediction day to another, the atmospheric predictors selected in the regression stage and the value of the corresponding regression coefficients can vary from one prediction day to another. The model allows thus for a?day-to-day adaptive and tailored downscaling. It can also reveal specific predictors for peculiar and non-frequent weather configurations.
机译:统计缩小模型(SDMS)通常用于生产来自大型大气信息的当地天气情况。 SDM包括基于a的传递函数,其基于a的统计链路识别出从当地天气和一个大规模预测器的一组的观察结果。由于驾驶表面天气随时间变化的物理过程,最相关的预测器和回归链接也可能随时间变化。这是众所周知的,例如沉淀,因此在数据的一些季节性分层之后经常估计链路。在这项研究中,我们提出了一个?两级模拟/回归模型,其中回归链路估计了当前预测日的大气类似物。大气类似物由1000和500℃的地球势高度的领域鉴定。对于回归阶段,两个广义的线性模型进一步用于模拟降水发生的概率和非零降水量的分布。评估两阶段模型的法国小规模降水的概率预测。它明显改善了对沉淀发生和量的预测的技能。随着模拟日从一个预测日变化到另一个预测日,在回归阶段中选择的大气预测器和相应的回归系数的值可以从一个预测日到另一日不同。因此,该模型允许用于一个日常自适应和量身定制的折射。它还可以揭示特定的预测因子,用于特殊和非频繁天气配置。

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