Advancing Characterization and Modeling of Space-Time Correlation Structure and Marginal Distribution of Short-Duration Precipitation

被引:5
作者
Mascaro, Giuseppe [1 ,4 ]
Papalexiou, Simon Michael [2 ]
Wright, Daniel B. [3 ]
机构
[1] Arizona State Univ, Sch Sustainable Engn & Built Environm, Tempe, AZ USA
[2] Univ Calgary, Civil Engn, Calgary, AB, Canada
[3] Univ Wisconsin Madison, Civil & Environm Engn, Madison, WI USA
[4] Arizona State Univ, Sch Sustainable Engn & Built Environm, 777 E Univ Dr, Tempe, AZ 85287 USA
基金
美国国家科学基金会;
关键词
Short-duration precipitation; Multisite stochastic rainfall modeling; Space-time rainfall correlation; Rainfall probability distributions; SCALE RAINFALL VARIABILITY; UNCERTAINTY; EXTREMES; STORMS; BASIN;
D O I
10.1016/j.advwatres.2023.104451
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
The statistical characterization of precipitation (P) at short durations (& LE; 24 h) is crucial for practical and scientific applications. Here, we advance the knowledge of and ability to model the space-time correlation structure (STCS) and marginal distribution of short-duration P using a network of rain gages in central Arizona with one of the largest densities and spatial coverages in the world. We separately analyze summer and winter P sampled at multiple durations, At, from 0.5 to 24 h. We first identify an analytical model and a three-parameter distribution that robustly capture the empirical STCS and marginal distribution of P, respectively, across At's. We then conduct Monte Carlo experiments consisting of multisite stochastic simulations of P time series to explore the spatial and seasonal variability of these properties. Significant seasonal differences emerge, especially at low At. Summer (winter) P exhibits weak (strong) correlation structure and heavy- (light-)tailed distributions resulting from short-lived, isolated thunderstorms (widespread, long-lasting frontal systems). The STCS of P is most likely homogeneous and isotropic except for winter at At & GE; 3 h, where anisotropy could be introduced via the motion of frontal storms. The spatial variability of the marginal distribution is reproduced by a regional parameterization dependent on elevation in all cases except, again, for winter at At & GE; 3 h where additional factors are needed to explain the variability of the mean P intensity. This work provides insights to improve stochastic P models and validate convection-permitting models used to investigate the mechanisms driving changes in short-duration P.
引用
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页数:18
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