4.6 Article

Spatial and temporal scaling of sub-daily extreme rainfall for data sparse places

Journal

CLIMATE DYNAMICS
Volume 60, Issue 11-12, Pages 3577-3596

Publisher

SPRINGER
DOI: 10.1007/s00382-022-06528-2

Keywords

Regional climate downscaling; Extreme rainfall; Intensity-duration-frequency; Tropics; Flood

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Global efforts to improve water, drainage, and sanitation services face challenges due to lack of hydrometeorological data and uncertainty about climate change. This paper presents a novel procedure for downscaled heavy rainfall simulation using media reports and introduces a three-step workflow to spatially and temporally scale rainfall data. The methods are applied to two cities in East Africa and demonstrate the reliability of scaling Gumbel parameters to different durations.
Global efforts to upgrade water, drainage, and sanitation services are hampered by hydrometeorological data-scarcity plus uncertainty about climate change. Intensity-duration-frequency (IDF) tables are used routinely to design water infrastructure so offer an entry point for adapting engineering standards. This paper begins with a novel procedure for guiding downscaling predictor variable selection for heavy rainfall simulation using media reports of pluvial flooding. We then present a three-step workflow to: (1) spatially downscale daily rainfall from grid-to-point resolutions; (2) temporally scale from daily series to sub-daily extreme rainfalls and; (3) test methods of temporal scaling of extreme rainfalls within Regional Climate Model (RCM) simulations under changed climate conditions. Critically, we compare the methods of moments and of parameters for temporal scaling annual maximum series of daily rainfall into sub-daily extreme rainfalls, whilst accounting for rainfall intermittency. The methods are applied to Kampala, Uganda and Kisumu, Kenya using the Statistical Downscaling Model (SDSM), two RCM simulations covering East Africa (CP4 and P25), and in hybrid form (RCM-SDSM). We demonstrate that Gumbel parameters (and IDF tables) can be reliably scaled to durations of 3 h within observations and RCMs. Our hybrid RCM-SDSM scaling reduces errors in IDF estimates for the present climate when compared with direct RCM output. Credible parameter scaling relationships are also found within RCM simulations under changed climate conditions. We then discuss the practical aspects of applying such workflows to other city-regions.

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