TECHNICAL NOTES
Nov 1, 2006

Spatial Uncertainty Modeling of Climate Processes for Extreme Hydrogeomorphological Events Hazard Monitoring

Publication: Journal of Environmental Engineering
Volume 132, Issue 11

Abstract

The growing concern of the possible impact of natural disasters and extreme events on the environment has recently created new demands for information from, and assessment by, environmental engineers and climatologists. Mediterranean river basins encompass a diverse range of valley and floodplain environments and are affected by many different processes, such as hydroclimate, land-use, catchment geology, and relief. The objective of this paper is to develop a methodology for exploratory rainstorms data analysis and uncertainty estimation in regional hydrogeomorphological frequency analysis (HFA). A general framework is proposed for designing spatial variability of rainstorms with assigned return periods (T) inducing multiple damaging hydrogeomorphological events in the Campania region, south Italy. To this end, the analysis of precipitation, involving means techniques of regional HFA and geostatistical theory integrated approaches, is a subject of great interest. However, the hydrogeomorphological consequences depend on complex interactions between extreme precipitation and torrential characteristics of the landscape. In Mediterranean environments, climatic fluctuations in hydrological regime, especially those exceeding rain thresholds for an acceptable range of flexibility, can be the main causes of relevant hydrogeomorphological impacts. An algorithm for the characterization of this impact termed with the acronym DRHI (Design Rainstorms Hazard Index) in this paper is presented first. Next, the continuous DRHI data are converted at each location using a binary variable indicator transform based on critical thresholds. In the third step, the expansion of DRHI-soft information from point to landscapes were assessed geostatistically using the records of 70 rain stations of the Department of Civil Protection established by Regional Monitoring Networks. In this way, threshold values for extreme hydrogeomorphological impacts were selected based on geographical distribution patterns of precipitation maxima with a duration of 3h for a return period of 10, 20, and 50 years. Moreover, the map-based method provides the identification where future infill sampling should be focused in support of more precise characterization.

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Acknowledgments

The writer gratefully acknowledges the two anonymous reviewers for providing helpful comments. N.D. is also very grateful to Dr. Mauro Biafora, Dr. Matteo Gentilella, Giuseppe Benassai (Hydropluviometric Monitoring Network of Campania Region, Department of Civil Protection and Programming on Territory—Naples) and Dr. Mario Russo that facilitated the data collection on the precipitation series used in this work, derived from the former Servizio Idrografico e Mareografico Nazionale Italiano.

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Go to Journal of Environmental Engineering
Journal of Environmental Engineering
Volume 132Issue 11November 2006
Pages: 1530 - 1538

History

Received: Jan 21, 2005
Accepted: Apr 10, 2006
Published online: Nov 1, 2006
Published in print: Nov 2006

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Nazzareno Diodato
Monte Pino Research Observatory on Climate and Landscape, 82100 Benevento Italy; and GTOS\TEMS Network-Terrestrial Ecosystem Monitoring Sites (FAO-United Nations). E-mail: [email protected]

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