Search results for " sistemazioni idraulico-forestali"

showing 10 items of 760 documents

L’evento alluvionale dell’Ottobre 2009 nel Messinese

2010

GiampilieriSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEvento alluvionale
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A simple method to directly retrieve reference evapotranspiration from geostationary satellite images

2013

Abstract Application of FAO-56 methodology for the assessment of reference evapotranspiration, ET 0 , is challenging in areas of the world with sparse meteorological network stations. For this reason alternative procedures using remotely observed data have been proposed in the literature. In this work, a simplified version of the Makkink approach [J. Inst. Wat. Eng. 11: 277–288, 1957] was tested in a typical Mediterranean environment (Sicily, Italy). The implemented Makkink approach (MAK) uses remotely estimated solar radiation derived from Meteosat Second Generation (MSG) satellite data and in situ observations of air temperature to assess ET 0 at daily time scale. Alternatively, taking ad…

Global and Planetary ChangeMeteorologySettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaElevationOrographyReference evapotranspiration MSG geostationary satellite Mediterranean environmentManagement Monitoring Policy and LawSeasonalitymedicine.diseaseRegressionGeographyApproximation errorEvapotranspirationGeostationary orbitmedicineSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliComputers in Earth SciencesScale (map)Reference evapotranspiration MSG geostationary satellite Mediterranean environmentEarth-Surface Processes
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Measuring Rainfall Kinetic Power in Two Sicilian Experimental Areas by Drop-Size Distribution Data

2023

The rainfall kinetic energy, which affects soil erosion processes, can be calculated by the drop-size distribution (DSD) and falling velocity. This study presents the outcomes derived by the DSDs recorded with the same optical disdrometer in two experimental areas, located in Sicily (southern Italy). Specifically, the DSDs were recorded from March 2017 to December 2019 at Sparacia and from June 2006 to April 2014 at Palermo. The aims of this paper are both to compare the DSDs for the two sites and to evaluate the applicability of Gamma theoretical distribution. Moreover, the relations of rainfall kinetic power vs. rainfall intensity are assessed. Differences in DSDs, especially for rainfall…

Global and Planetary Changeerosion modelsrainfall kinetic energyEcologyerosion modeldrop-size distributionrainfall erosivitysoil lossSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalisoil loNature and Landscape ConservationLand
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A rational runoff coefficient for a revisited rational formula

2019

The Rational Formula (RF) is probably the most frequently applied equation in practical hydrology to compute the peak discharge, due to its simplicity and effective compromise between theory and data availability. Thus, after more than a century, the estimation of peak discharge through the RF is still an important and challenging issue in hydrology. The RF assumes response linearity and sometimes assumes that the return period does not depend on the runoff coefficient and neglects the time to ponding and the antecedent moisture condition. Moreover, the RF requires the critical duration of rainfall and the runoff coefficient to be estimated, both of which are highly controversial. This pape…

Green-Ampt modelmedia_common.quotation_subject0208 environmental biotechnologyhydrological response02 engineering and technology020801 environmental engineeringRunoff coefficientHydrology (agriculture)rational formulahillslope scaleSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliApplied mathematicskinematic wave modelSimplicityrunoff coefficientWater Science and Technologymedia_commonMathematicsHydrological Sciences Journal
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Discussion of “Soil Water Retention Characteristics of Vertisols and Pedotransfer Functions Based on Nearest Neighbor and Neural Networks Approaches …

2013

HYDRAULIC PROPERTIESArtificial neural networkPREDICTIONSWRCSoil scienceSoil Water Retention Curve Soil Shrinkage Characteristic CurveVertisolHYDRAULIC PROPERTIES; SHRINKAGE; PREDICTION; SWRC; ANNAgricultural and Biological Sciences (miscellaneous)k-nearest neighbors algorithmPedotransfer functionSoil waterSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSHRINKAGEANNWater Science and TechnologyCivil and Structural EngineeringMathematics
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EXPERIMENTAL STUDY OF RILL FLOW RESISTANCE AT PLOT SCALE

2021

I processi erosivi costituiscono un rilevante problema ambientale con impatto anche di tipo socioeconomico. Infatti, questi processi determinando l’asportazione degli strati superficiali di suolo, causano la riduzione della fertilità e produttività del suolo, e hanno un considerevole impatto sulla biodiversità. La perdita di suolo dovuta all’erosione idrica è un fenomeno naturale ed inevitabile, che può divenire intollerabile in condizioni particolari che spesso dipendono da fattori antropici (Di Stefano e Ferro, 2016). I processi di erosione idrica sono generalmente caratterizzati dall’erosione interrill o rill. Nelle aree interrill, caratterizzate da correnti overland, il processo erosivo…

HYDRAULICSRILLSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliPLOTSOIL EROSIONFLOW RESISTANCE
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Uso del modello di simulazione HYDRUS-2D per lo studio dei processi di trasporto di soluti nel terreno

2008

HYDRUS – 2D Trasporto soluti Metalli pesantiSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Beerkan Estimation of Soil Transfer parameters (BEST) across soils and scales

2019

Abstract Theories and models used in soil hydrological sciences rely on the knowledge of the spatially and temporally variable soil hydraulic properties, i.e. the water retention and hydraulic conductivity curves. Obtaining reliable experimental information on these curves for an area of interest is not easy and it still remains a challenge for soil scientists. In 2006, a simple and physically based methodology was proposed to completely characterize the soil using a single ring infiltration experiment in the field and determination of soil particle size distribution, initial and final soil water content and dry soil bulk density. This methodology, named BEST – Beerkan Estimation of Soil Tr…

Heterogeneous soil010504 meteorology & atmospheric sciencesSoil textureHydraulic conductivity0207 environmental engineeringDual-permeability soilSoil science02 engineering and technology01 natural sciencesSealed soilHydraulic conductivityDry soilSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali020701 environmental engineeringComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesWater Science and TechnologyBEST methodInfiltrationArea of interest15. Life on landBulk density6. Clean waterWater repellencyInfiltration (hydrology)Soil waterEnvironmental science[SDE.BE]Environmental Sciences/Biodiversity and Ecology
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Modelling rainfall interarrival times and rainfall depths at daily scale

2023

Analysis of daily rainfall data, and subsequent modelling of some derived variables concerning rainfall, is fundamental in different areas such as agricultural, ecological, and engineering disciplines. A way of studying the alternance of consecutive rainy days (wet spells) and no-rainy days (dry spells) is through the interarrival time (IT), which is the time elapsed between two consecutives rainy days. If we suppose that IT observations are independent and identically distributed (i.i.d.), ITs are usually modelled through a renewal processes. The simplest renewal process is the Bernoulli process with ITs geometrically distributed. The need to suppose a non-constant probability of rain brin…

Hurwitz-Lerch-Zeta distribution interarrival times daily rainfallSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Applying a probabilistic model of rainfall and snow days occurrence to daily series recorded in NW Italy.

2014

Daily precipitation records exist spanning several decades. A valuable amount of climatic information exists in the time-series of interarrival times (IT), defined as the succession of times (number of days) elapsed from a rainy (or snowy) day to the one immediately preceding it.In a previous work, Agnese et al. (2014) have been successfully tested some probabilistic modelling of rain occurrence on Sicily rainfall data; particularly, the better fitting of IT’s observed frequencies was obtained by 3-parameter Lerch-series distribution. In this work thisdistribution is tested on 70 years of 20 precipitation time-series taken in the North-West Italy, both in the plain and in the mountains, up …

Hurwitz–Lerch Zeta probability distributions Inter-arrival times Rain probabilitySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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