Titlebook: Storminess and Environmental Change; Climate Forcing and Nazzareno Diodato,Gianni Bellocchi Book 2014 Springer Science+Business Media Dord

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Spatial Pattern Probabilities Exceeding Critical Threshold of Annual Mean Storm-Erosivity in Euro-Meature for land-and-soil conservation-and-planning of the river basins. This work illustrates a spatial modelling study of rainstorm aggressiveness to assess downscaling in the erosive rainfall climatic classification across Euro-Mediterranean regions. Rainfall erosivity was estimated by the R–climat

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Landscape Scales of Erosive Storm Hazard Across the Mediterranean Regionrd in the Mediterranean region. From long-term average erosivity values, it was observed that large erosive rainfalls tend to occur especially in late summer, confined to continental areas, and autumn, along the Mediterranean coasts and near-to-coast reliefs. Rainfall intensity anomalies registered

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Storm-Erosivity Model for Addressing Hydrological Effectiveness in Francef the 95th percentile) are used to estimate decadal-scale rainfall–runoff erosivity values compatible with the Universal Soil Loss Equation and its revision – (R)USLE. The model meets the need of estimating rainfall-runoff erosivity when sub-daily extremes rainfall data are missing. The test region

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Modelling Long-Term Storm Erosivity Time-Series: A Case Study in the Western Swiss Plateaulogical events worldwide. The present paper proposes advances in our understanding of the hydroclimatological processes and their associated modelling requirements that can be useful in both climate simulation and extremes reconstruction. The novel model . (Complexity-reduced Storm Erosivity Model)

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Temporal and Spatial Patterns in Design–Storm Erosivity Over Sicily RegionMediterranean Central Area (MCA). Starting from the long-term mean erosivity spatial pattern, a downscaling approach to estimate design-storm erosivity was exploited with the aim to map the climate hazard over Sicily referred to 5- and 20-years return periods during the nominal period 1950–1998. The