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首页> 外文期刊>Water resources research >A hierarchical Bayesian regional model for nonstationary precipitation extremes in Northern California conditioned on tropical moisture exports
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A hierarchical Bayesian regional model for nonstationary precipitation extremes in Northern California conditioned on tropical moisture exports

机译:基于热带水分出口的北加利福尼亚州非平稳降水极端事件的分级贝叶斯区域模型

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Warm, moist, and longitudinally confined tropical air masses are being linked to some of the most extreme precipitation and flooding events in the midlatitudes. The interannual frequency and intensity of such atmospheric rivers (ARs), or tropical moisture exports (TMEs), are connected to the risk of extreme precipitation events in areas where moisture convergence occurs. This study presents a nonstationary, regional frequency analysis of precipitation extremes in Northern California that is conditioned on the interannual variability of TMEs entering the region. Parameters of a multisite peaks-over-threshold model are allowed to vary conditional on the integrated moisture delivery from TMEs over the area. Parameters are also related to time-invariant, local characteristics to facilitate regionalization to ungaged sites. The model is developed and calibrated in a hierarchical Bayesian framework to support partial pooling and enhance regionalization skill. The model is cross validated along with two alternative, increasingly parsimonious formulations to assess the additional skill provided by the covariates. Climate diagnostics are also used to better understand the instances where TMEs fail to explain variations in rainfall extremes to provide a path forward for further model improvement. The modeling structure is designed to link seasonal forecasting and long-term projections of TMEs directly to regional models of extremes used for risk estimation. Results suggest that the inclusion of TME-based information greatly improves the characterization of extremes, particularly for their frequency of occurrence. Diagnostics indicate that the model could be further improved by considering an index for frontal systems as an additional covariate.
机译:温暖,潮湿和纵向受限的热带气团与中纬度地区某些最极端的降水和洪水事件有关。这种大气河流(AR)或热带湿气出口(TME)的年际频率和强度与发生湿气收敛的地区发生极端降水事件的风险有关。这项研究提出了北加州极端降水的非平稳区域频率分析,该分析以进入该地区的TME的年际变化为条件。允许多站点阈值峰值模型的参数根据区域内TME的综合水分输送而变化。参数还与时不变的局部特征相关,以促进对未使用部位的区域化。该模型是在分层贝叶斯框架中开发和校准的,以支持部分合并和增强区域化技能。该模型与两个替代的,日益简化的公式进行了交叉验证,以评估协变量提供的其他技能。气候诊断还用于更好地理解TME无法解释极端降雨的情况,从而为进一步改进模型提供了一条途径。该建模结构旨在将TME的季节性预测和长期预测直接与用于风险估计的极端区域模型联系起来。结果表明,包含基于TME的信息极大地改善了极端现象的特征,特别是极端事件的发生频率。诊断表明,可以通过考虑额叶系统的索引作为附加协变量来进一步改善模型。

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