Spatial Modeling and Future Projection of Extreme Precipitation Extents

被引:0
|
作者
Zhong, Peng [1 ]
Brunner, Manuela [2 ,3 ,4 ]
Opitz, Thomas [5 ]
Huser, Raphael [6 ]
机构
[1] Univ New South Wales, Sch Math & Stat, Data Sci Hub, Sydney, Australia
[2] Swiss Fed Inst Technol, Inst Atmospher & Climate Sci, Zurich, Switzerland
[3] WSL Inst Snow & Avalanche Res SLF, Davos, Switzerland
[4] Climate Change Extremes & Nat Hazards Alpine Reg R, Davos, Switzerland
[5] INRAE, Biostat & Spatial Proc, Avignon, France
[6] KAUST, Stat Program, Comp Elect & Math Sci & Engn CEMSE Div, Thuwal 239556900, Saudi Arabia
基金
澳大利亚研究理事会;
关键词
Climate change; Extreme event; Extreme-value theory; Peaks over threshold; <italic>r</italic>-Pareto process; Spatial dependence; RAINFALL EVENTS; TEMPERATURE; DEPENDENCE; STORMS; PEAKS;
D O I
10.1080/01621459.2024.2408045
中图分类号
O21 [概率论与数理统计]; C8 [统计学];
学科分类号
020208 ; 070103 ; 0714 ;
摘要
Extreme precipitation events with large spatial extents may have more severe impacts than localized events as they can lead to widespread flooding. It is debated how climate change may affect the spatial extent of precipitation extremes, whose investigation often directly relies on simulations of precipitation from climate models. Here, we use a different strategy to investigate how future changes in spatial extents of precipitation extremes differ across climate zones and seasons in two river basins (Danube and Mississippi). We rely on observed precipitation extremes while exploiting a physics-based average-temperature covariate, enabling us to project future precipitation extents based on projected temperatures. We include the covariate into newly developed time-varying r-Pareto processes using suitably chosen spatial risk functionals r. This model captures temporal non-stationarity in the spatial dependence structure of precipitation extremes by linking it to the temperature covariate, derived from reanalysis data (ERA5-Land) for model calibration and from bias-corrected climate simulations (CMIP6) for projections. Our results show an increasing trend in the margins, with both significantly positive or negative trend coefficients depending on season and river (sub-)basin. During major rainy seasons, the significant trends indicate that future spatial extreme events will become relatively more intense and localized in several sub-basins. Supplementary materials for this article are available online, including a standardized description of the materials available for reproducing the work.
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页数:16
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