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

periodontitis

Extreme Rainfalls in the Mediterranean Areass, it has been evidenced only a significant increase of “moderate” events (whole basin) and a meanwhile decrease of “strong” events (West). On the other hand, the observed positive trends of classes “moderate” and “strong” for the East part of the basin should be confirmed by a richer dataset refer

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synovium

扩张

Monthly Erosive Storm Hazard Within River Basins of the Campania Region, Southern Italya more random occurrence in other periods of the year. Taking SISEM model very few and easy retrievable data into account, it is desirable to extend its use of sites without any pluviograph data for time and spatial interpolation purposes over peninsular Central and Southern Italy.

敌手

Storm-Erosivity Model for Addressing Hydrological Effectiveness in Franceogy. In addition, the inclusion of a site-specific elevation term allowed to account for the specific features of mainland France. Once parameterized to capture decadal rainfall–runoff erosivity variability over the test area, the DREMM-F was run to produce the temporal pattern of rainfall-runoff er

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大方不好

Temporal and Spatial Patterns in Design–Storm Erosivity Over Sicily Regionmaps for practical questions involving communication uncertainty in detecting erosive-prone areas. This approach provides a first exploration of critical areas and helps identify where future infill sampling should be focused in supporting a more precise characterization and conservation planning.

guardianship

Historical Reconstruction of Erosive Storms Driving Damaging Hydrological Events in the Bonea Basin,ESAM (Cumulative Erosive Storm Anomalies per Annum) from a previous erosivity anomalies equation and evaluated against erosivity data compatible with the RUSLE scheme. The historical climatology of the Bonea basin has shown pronounced interannual and interdecadal variations dependent on multi-decada

ILEUM

Triggering Conditions and Runout Simulation of the San Mango sul Calore Debris Avalanche, Southern Iut landslide motion we performed a dynamic analysis using the model DAN3D to simulate the landslide mass. The rheological parameters used to simulate the event have been obtained from laboratory tests and through trial and error site-specific calibration.

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