0000000000940040

AUTHOR

Carmelo Agnese

showing 56 related works from this author

Scaling properties of topologically random channel networks

1996

Abstract The analysis deals with the scaling properties of infinite topologically random channel networks (ITRNs) fast introduced by Shreve (1967, J. Geol. , 75: 179–186) to model the branching structure of rivers as a random process. The expected configuration of ITRNs displays scaling behaviour only asymptotically, when the ruler (or ‘yardstick’) length is reduced to a very small extent. The random model can also reproduce scaling behaviour at larger ruler lengths if network magnitude and diameter are functionally related according to a reported deterministic rule. This indicates that subsets of rrRNs can be scaling and, although rrRNs are asymptotically plane-filling due to the law of la…

Discrete mathematicsDimension (vector space)YardstickLaw of large numbersStochastic processStructure (category theory)Magnitude (mathematics)Statistical physicsScalingWater Science and TechnologyMathematicsCommunication channelJournal of Hydrology
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Actual evapotranspiration assessment by means of a coupled energy/hydrologic balance model: Validation over an olive grove by means of scintillometry…

2010

Summary A coupled energy/hydrologic model was applied to simulate the exchange of energy and water in the soil–plant-atmosphere system (SPA). The model, which uses a “two-source” approach to estimate the energy fluxes, and the “force-restore” approach to represent the water balance, was validated by means of evapotranspiration measurements collected via scintillometry and soil moisture measurements collected via time domain reflectometry (TDR) in a Sicilian olive grove. The comparison between measured and estimated fluxes values at an hourly scale showed good agreement. Additional comparisons on a daily timescale confirmed the model’s applicability for quantifying crop water requirements. A…

Actual evapotranspirationHydrologyScintillometer measurementsMoistureScale (ratio)Settore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaEnergy balanceScintillometer measurementHydrologic balanceWater balanceHydrology (agriculture)EvapotranspirationActual evapotranspiration; Scintillometer measurements; Olive grove; Surface energy fluxes; Hydrologic balanceSoil waterOlive groveSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceSurface energy fluxesSurface energy fluxeWater contentWater Science and TechnologyJournal of Hydrology
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Comparing Physical Quality of Forest and Pasture Soils in a Sicilian Watershed

2011

Forest and pasture soils should have differing properties due, for example, to differing root characteristics or livestock trampling rates, but contradictory results are reported in the literature. The surface soil physical and hydraulic properties of five forest and pasture sites were determined in a Sicilian watershed. In general, forest soils had a significantly lower bulk density, b (by 17 to 35%), and a higher field saturated hydraulic conductivity, Kfs (by a factor of 3.4-11.5) than pasture soils. Differences between water retention characteristics of forest and pasture soils were low when high levels of organic matter, OM, content (> 7.1%) were detected for both land uses. The mean …

geographysoil physical qualityWatershedgeography.geographical_feature_categoryAgroforestrymedia_common.quotation_subjectSoil SciencePasturelanguage.human_languageSoil waterlanguageSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceQuality (business)SFH techniqueSicilianmedia_commonSoil Science Society of America Journal
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A simple model of hillslope response for overland flow generation

2001

This paper deals with the derivation of the hydrological response of a hillslope on the assumption of quick runoff by surface runoff generation. By using the simple non-linear storage based model, first proposed by Horton, an analytical solution of the overland flow equations over a plane hillslope was derived. This solution establishes a generalization for different flow regimes of Horton's original solution, which is valid for the transitional flow regime only. The solution proposed was compared successfully with that of Horton and, for the turbulent flow regime, to the one derived from kinematic wave theory. This solution can be applied easily to both stationary and non-stationary rainfa…

Kinematic waveMathematical modelMeteorologyFlow (mathematics)Plane (geometry)TurbulenceGeneralizationMechanicsFunction (mathematics)Surface runoffWater Science and TechnologyMathematicsHydrological Processes
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Quick and Slow Components of the Hydrologic Response at the Hillslope Scale

2016

It is widely recognized that the Hortonian mechanism of runoff generation occurs in arid and semi-arid regions, generally characterized by high rainfall intensity on soils exhibiting low infiltrabilities. Differently, in steeply sloping forested watersheds in humid climates, by infiltrating through a highly permeable upper soil horizon, water moves beneath the soil surface determining a slow response. However, in most real cases, for example when in arid regions mountain forested areas take place, both (quick and slow) runoff generation processes coexist and together contribute to the hydrologic hillslope response. In this paper, based on analytical solutions of the hydrologic response, ins…

HydrologySubsurface stormflowGamma probability density function0208 environmental biotechnologyhillslope scale overland flow subsurface stormflow instantaneous response function gamma probability density function02 engineering and technologySoil surfaceAgricultural and Biological Sciences (miscellaneous)Arid020801 environmental engineeringInstantaneous response functionOverland flowSoil waterEnvironmental scienceSoil horizonSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSlow responseHillslope scaleScale (map)Surface runoffIntensity (heat transfer)Water Science and TechnologyCivil and Structural Engineering
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Overland flow generation on hillslopes of complex topography: analytical Solutions

2007

The analytical solution of the overland flow equations developed by Agnese et al. (2001; Hydrological Processes15: 3225–3238) for rectangular straight hillslopes was extended to convergent and divergent surfaces and to concave and convex profiles. Towards this aim, the conical convergent and divergent surfaces are approximated by a trapezoidal shape, and the overland flow is assumed to be always one-dimensional. A simple ‘shape factor’ accounting for both planform geometry and profile shape was introduced: for each planform geometry, a brachistochrone profile was obtained by minimizing a functional containing a slope function of the profile. Minima shape factors are associated with brachist…

brachistochroneRegular polygonGeometryConical surfaceFunction (mathematics)analytical solutionMaxima and minimaoverland flowSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestaliconvergent and divergent hillslopeShape factorDivergence (statistics)Surface runoffoverland flow; convergent and divergent hillslopes; concave and convex profiles; analytical solution; brachistochroneconcave and convex profileBrachistochrone curveGeologyWater Science and Technology
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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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Modelling the Frequency of Interarrival Times and Rainfall Depths with the Poisson Hurwitz-Lerch Zeta Distribution

2022

The Poisson-stopped sum of the Hurwitz–Lerch zeta distribution is proposed as a model for interarrival times and rainfall depths. Theoretical properties and characterizations are investigated in comparison with other two models implemented to perform the same task: the Hurwitz–Lerch zeta distribution and the one inflated Hurwitz–Lerch zeta distribution. Within this framework, the capability of these three distributions to fit the main statistical features of rainfall time series was tested on a dataset never previously considered in the literature and chosen in order to represent very different climates from the rainfall characteristics point of view. The results address t…

Statistics and ProbabilityHurwitz-Lerch Zeta distribution; log-concavity; compound poisson distribution; one inflated model; moment; simulated annealingHurwitz-Lerch zeta distributionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliStatistical and Nonlinear Physicssimulated annealinglog-concavityone inflated modelAnalysiscompound poisson distributionmoment
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Estimation of Daily Solar Radiation from Measured Air Temperature Extremes in the Mid-Mediterranean Area

2012

AbstractDaily solar radiation Rs at ground level is a necessary input variable required for the evaluation of evapotranspiration and crop growth, development, and yield-simulation models. Nevertheless, it is measured in few weather stations and at many locations it is not observed; also, available Rs temporal series are generally no longer than a few years. A valid surrogate of Rs measurement is the diurnal air-temperature range (ΔT); indeed, ΔT is inversely proportional to cloudiness and therefore could be a good indicator of atmospheric transmittance. As opposed to Rs, daily maximum and minimum air temperatures are measured at many locations and their observations in developed countries b…

EstimationMediterranean seaInfrared windowCloud coverAir temperatureClimatologyEvapotranspirationRange (statistics)Environmental scienceRadiationAgricultural and Biological Sciences (miscellaneous)Water Science and TechnologyCivil and Structural EngineeringJournal of Irrigation and Drainage Engineering
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Estimation of actual evapotranspiration of Mediterranean perennial crops by means of remote-sensing based surface energy balance models

2009

Abstract. Actual evapotranspiration from typical Mediterranean crops has been assessed in a Sicilian study area by using surface energy balance (SEB) and soil-water balance models. Both modelling approaches use remotely sensed data to estimate evapotranspiration fluxes in a spatially distributed way. The first approach exploits visible (VIS), near-infrared (NIR) and thermal (TIR) observations to solve the surface energy balance equation whereas the soil-water balance model uses only VIS-NIR data to detect the spatial variability of crop parameters. Considering that the study area is characterized by typical spatially sparse Mediterranean vegetation, i.e. olive, citrus and vineyards, alterna…

SEBALWater flowEnergy balancelcsh:Technologylcsh:TD1-1066remote sensingWater balanceSEBALEvapotranspirationSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalilcsh:Environmental technology. Sanitary engineeringTSEBlcsh:Environmental sciencesRemote sensinglcsh:GE1-350Evapotranspiration remote sensing SEBAL TSEB SWAPEvapotranspirationtemperaturalcsh:TSWAPlcsh:Geography. Anthropology. RecreationHyperspectral imaginglcsh:GSoil watertelerilevamentoEnvironmental scienceSpatial variabilityevapotraspirazioneHydrology and Earth System Sciences
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Estimation of Mediterranean crops evapotranspiration by means of remote-sensing based models

2009

Abstract. Actual evapotranspiration from typical Mediterranean crops has been assessed in a Sicilian study area by using Surface Energy Balance and Agro-Hydrological models. Both modelling approaches require remotely sensed data to estimate evapotranspiration fluxes in a spatially distributed way. The first approach exploits visible (VIS), near-infrared (NIR) and thermal (TIR) observations to solve the surface energy balance equation. To this end two different schemes have been tested: the two-sources TSEB model, where soil and vegetation components of the surface energy balance are treated separately, and the widely used one-source SEBAL model, where soil and vegetation are considered as a…

HydrologyMediterranean climateEstimationSEBALEvapotranspirationEvapotranspiration remote sensing SEBAL TSEB SWAPSWAPremote sensingSEBALRemote sensing (archaeology)EvapotranspirationEnvironmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliTSEBRemote sensing
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Influence of the rainfall measurement interval on the erosivity determinations in the Mediterranean area

2006

Summary The single-storm erosion index, EI, of the USLE and RUSLE models may vary appreciably with the rainfall measurement interval, Δ t . However, the effect of Δ t on EI has not been investigated in the Mediterranean area. Approximately 700 erosive events and 1.5 years of rainfall energies measured by a rainfall impact measurement device were used to evaluate the effect of the rainfall measurement interval (5 min ⩽ Δ t  ⩽ 60 min) on the erosivity determinations in the Mediterranean semi-arid area of Sicily. According to both literature and practical considerations, a reference time interval equal to 15 min was used in this investigation. Hourly rainfall data led to an appreciable underes…

Mediterranean climateHydrologyStormAtmospheric sciencesMediterranean areaR-value (insulation)USLE/RUSLER-factorsoil erosion; USLE/RUSLE; R-factor; rainfall kinetic energy; Mediterranean areaSoil lossrainfall kinetic energySoil waterMaximum differenceSoil erosionErosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliMediterranean areaEnvironmental scienceWater Science and TechnologyJournal of Hydrology
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Comparison of SWAP and FAO Agro-Hydrological Models to Schedule Irrigation of Wine Grapes

2012

This paper compares two agro-hydrological models that are used to schedule irrigation of a typical Mediterranean crop. In particular, a comparison between the Food and Agriculture Organization (FAO) model, which uses a black box approach, and the soil-water-atmosphere-plant (SWAP) model, which is based on the numerical analysis of Richards' equation, are shown for wine grape. The comparison was carried out for the 2005 and 2006 irrigation seasons and focused on hydrological balance components and on soil water contents. Next, the ordinary scheduling parameters were identified so that the performance of the two models, which aimed to evaluate the seasonal water requirements and the irrigatio…

HydrologyIrrigationFAO-56 agro-hydrological modelbusiness.industryHydrological modellingDeficit irrigationIrrigation schedulingSWAP MODEL; Agro-hydrological models; Irrigation Scheduling — Wine grape; FAO-56 agro-hydrological modelAgricultural engineeringAgro-hydrological modelsSWAP MODELAgricultural and Biological Sciences (miscellaneous)Wine grapeAgro-hydrological models FAO 56 SWAP Irrigation Scheduling Wine grape.Irrigation Scheduling — Wine grapeAgricultureEvapotranspirationSoil waterSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental sciencebusinessWater Science and TechnologyCivil and Structural EngineeringJournal of Irrigation and Drainage Engineering
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Modelling the frequency distribution of inter-arrival times from daily precipitation time-series in North-West Italy

2018

Abstract The discrete three-parameter Lerch distribution is used to analyse the frequency distribution of inter-arrival times derived from 26 daily precipitation time-series, collected by stations located throughout a 28,000 km2 area in North-West Italy (altitudes ranging from 113 m to 2,170 m a.s.l.). The precipitation regime of these Alpine regions is very different (latitude 44.5 to 46.5 N) from the typical Mediterranean precipitation regime of the island of Sicily (latitude 37 to 38 N), where the Lerch distribution has already been tested and whose results are compared. In order to verify the homogeneity of the precipitation time series, the Pettitt test was preliminarily performed. In …

Rainfall regimeSeries (stratigraphy)Water scarcity010504 meteorology & atmospheric sciencesInter-arrival timesbusiness.industry0208 environmental biotechnologyDistribution (economics)Dry spells02 engineering and technology01 natural sciences020801 environmental engineeringinter-arrival times Lerch probability distribution rainfall regime water scarcity wet spells and dry spellsDry spells; Inter-arrival times; Lerch probability distribution; Rainfall regime; Water scarcity; Wet spellsNorth westClimatologySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceWet spellsPrecipitationbusinessLerch probability distribution0105 earth and related environmental sciencesWater Science and TechnologyHydrology Research
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Statistical analysis of inter-arrival times of rainfall events for Italian Sub-Alpine and Mediterranean areas

2012

Abstract. In this work a set of time-series of inter-arrival times of rainfall events, at daily scale, was analysed, with the aim to verify the issue of increasing duration of dry periods. The set consists of 12 time-series recorded at rain gauges in 1926–2005, six of them belong to an Italian Sub-Alpine area (Piedmont) and six to a Mediterranean one (Sicily). In order to overcome the problem related to limited sample size for high values of inter-arrival times, the discrete probability polylog-series distribution was used to fit the empirical data from partial (20 yr) time-series. Moreover, a simple qualitative trend analysis was applied to some high quantiles of inter-arrival times as wel…

Mediterranean climateAtmospheric ScienceDistribution (economics)droughtlcsh:QC851-999MediterraneanSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliDuration (project management)lcsh:ScienceSub-Alpinedrought; statistical distributions; trendbusiness.industryEcological ModelingSettore ICAR/02 - Costruzioni Idrauliche E Marittime E Idrologiastatistical distributionsPollutionlcsh:QC1-999Trend analysistrendGeophysicsGeographySample size determinationClimatologyProbability distributionlcsh:Qlcsh:Meteorology. Climatologyrainfall inter-arrival timeScale (map)businesslcsh:PhysicsQuantileAdvances in Science and Research
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Probability Distribution of Peak Discharge at the Hillslope Scale Generated by Hortonian Runoff

2016

In this work, the probability distribution of peak discharge at the hillslope bottom is determined hypothesizing a prevalent Hortonian mechanism of runoff production for a given rainfall duration. As is well known, the probability distribution of peak discharge depends on the probability of both the rainfall event as well as that of the antecedent soil moisture conditions. In particular, the probability of the rainfall event is calculated according to the familiar rainfall duration-intensity-frequency approach, whereas the ecohydrological method from the literature is used here to define the probability of the antecedent soil moisture conditions. The latter depends on a set of parameters de…

Hydrology010504 meteorology & atmospheric sciencesScale (ratio)0208 environmental biotechnologySoil science02 engineering and technology01 natural sciencesAgricultural and Biological Sciences (miscellaneous)020801 environmental engineeringDischarge prorwhiiiiy distributionEnvironmental scienceProbability distributionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliHydrologic response Hillslope scale Discharge probability distribution Ecohydrological approachSurface runoffFeuhydrological approachHydrologie response: Hillslope scale0105 earth and related environmental sciencesWater Science and TechnologyCivil and Structural Engineering
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Modelling the occurrence of rainy days under a typical Mediterranean climate

2014

The statistical inference of the alternation of wet and dry periods in daily rainfall records can be achieved through the modelling of inter-arrival time-series, IT, defined as the succession of times elapsed from a rainy day and the one immediately preceding it. In this paper, under the hypothesis that ITs are independent and identically distributed random variables, a modelling framework based on a generalisation of the commonly adopted Bernoulli process is introduced. Within this framework, the capability of three discrete distributions, belonging to the Hurwitz–Lerch-Zeta family, to reproduce the main statistical features of IT time-series was tested. These distributions namely Lerch-se…

Independent and identically distributed random variablesHurwitz–Lerch Zeta probabilitydistributions Inter-arrival times Rain probabilitySeries (mathematics)Inter-arrival timesbusiness.industrySeasonalitymedicine.diseaseRain probabilityDistribution (mathematics)SkewnessHurwitz-Lerch Zeta probability distributionsStatisticsStatistical inferencemedicineSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliBernoulli processbusinessWater Science and TechnologyMathematicsSubdivisionAdvances in Water Resources
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AN ANALYTICAL SOLUTION OF KINEMATIC WAVE EQUATIONS FOR OVERLAND FLOW UNDER GREEN-AMPT INFILTRATION

2010

This paper deals with the analytical solution of kinematic wave equations for overland flow occurring in an infiltrating hillslope. The infiltration process is described by the Green-Ampt model. The solution is derived only for the case of an intermediate flow regime between laminar and turbulent ones. A transitional regime can be considered a reliable flow condition when, to the laminar overland flow, is also associated the effect of the additional resistance due to raindrop impact. With reference to the simple case of an impervious hillslope, a comparison was carried out between the present solution and the non-linear storage model. Some applications of the present solution were performed…

Mathematical modelTurbulenceMechanical Engineeringlcsh:SBioengineeringLaminar flowMechanicslcsh:S1-972Industrial and Manufacturing EngineeringKinematic wavePhysics::Fluid Dynamicslcsh:AgricultureInfiltration (hydrology)hydrologic response infiltration analytical solution kinematic wave equationsImpervious surfaceGeotechnical engineeringlcsh:Agriculture (General)Surface runoffGeologyJournal of Agricultural Engineering
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Combined use of eddy covariance and sap flow techniques for partition of ET fluxes and water stress assessment in an irrigated olive orchard

2013

Correct estimation of crop actual transpiration plays a key-role in precision irrigation scheduling, since crop growth and yield are associated to the water passing through the crop. Objective of the work was to assess how the combined use of micro-meteorological techniques (eddy covariance, EC) and physiological measurements (sap flow, SF) allows a better comprehension of the processes involving in the Soil–Plant–Atmosphere continuum. To this aim, an experimental dataset of actual evapotranspiration, plant transpiration, and soil water content measurements was collected in an olive orchard during the midseason phenological period of 2009 and 2010. It was demonstrated that the joint use of …

HydrologyPhenologyWater stressSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiafungiEddy covarianceOlivefood and beveragesSoil ScienceEddy covarianceEddy covariance; Flux partition; Olive; Sap flow; Water stressCrop coefficientFlux partitionSap flowEvapotranspirationSoil waterSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceDNS root zoneOrchardAgronomy and Crop ScienceEarth-Surface ProcessesWater Science and TechnologyTranspirationAgricultural Water Management
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Assessing agro-hydrological models to schedule irrigation for crops of Mediterranean Environment

2008

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSWAP FAO Scheduling irrigation
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Multiple Non-linear Reservoirs to Model Water Balance Components in Sandy Soils

2023

In the hydrologic literature, to model water flow in unsaturated soils, the Richards equation is usually applied, allowing the main components of the hydrologic cycle, as rainfall partitioning into surface runoff and infiltration, to be determined. The Richards equation is highly nonlinear, making very challenging to derive analytical solutions. Recently, for constant rainfall intensity, under the simplified hypothesis of gravity-driven infiltration, and by assuming a capacitance framework, a simplified solution of the Richards equation that considers the Brooks and Corey hydraulic conductivity function was suggested. By maintaining the assumption that the infiltration process is dominated …

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGravity-driven infiltration non-linear reservoirs sandy soils simplified solutions water balance components
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Effetti della copertura forestale sulle caratteristiche idrologiche del suolo

2009

densità apparente conducibilità idraulica boscoSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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About time of occurrence of rainy days for Mediterranean and (sub)-Alpine areas

2012

Settore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalirainfall day time-series intermittency inter-arrival time distribution Lerch probabilty distribution
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Determinazione delle proprietà idrauliche del suolo in una pendice naturale

2005

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Modeling olive orchard response to water stress and definition of critical thresholds of soil water status.

2011

Olive orchard Water stress functions Sap flows Leaf water potentialsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Sulla risposta idrologica di un versante a prevalente deflusso hortoniano

2005

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Sulla distribuzione dei tempi di inter-arrivo delle piogge

2012

La caratterizzazione probabilistica delle precipitazioni rappresenta un tema centrale in diverse aree di ricerca, come l'idrologia, la meteorologia, la climatologia, ed altre ancora, per le sue implicazioni sia teoriche sia pratiche. Un particolare interesse riguarda l’analisi della struttura probabilistica dei tempi di inter-arrivo delle piogge, alla scala giornaliera, che permette di inferire sulla probabilità della durata dei periodi di pioggia e dei periodi di siccità, dando conto sia della tendenza degli eventi di pioggia ad aggregarsi in cluster, che di quella alla persistenza dei periodi secchi. Nel presente lavoro, una siffatta analisi è stata condotta su alcune serie temporali di t…

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalidistribuzioni di probabilità Hurwitz-Lerch Zeta. tempi di inter-arrivo probabilità di pioggia
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Monitoraggio e modellazione agro-idrologica in ambiente mediterraneo:Applicazione ed indagini sperimentali.

2007

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Uso di modelli agro-idrologici per la gestione dell'irrigazione di colture arboree mediterranee

2008

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Delay times for saturation overland flow in forest soils

2007

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestaliinterception time to runoff forest hydrology
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Analisi regionale delle variazioni a lungo termine di grandezze climatiche in Sicilia

2007

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Stima delle componenti del flusso evapotraspirativo di un oliveto con l’uso congiunto delle tecniche Sap-Flow ed Eddy Covariance.

2011

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEvapotraspirazione COnsumo Idrico Traspirazione
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Spatial variability of dry spells duration statistical distributions

2014

Dry spells duration and its extent in space, is a key factor in water resources problems. In order to modelling the empirical distribution of dry spells (DS) frequencies observed in Sicily (i.e. in a typical Mediterranean climate), Agnese et al. (2014) successfully applied the two-parameter polylogarithm-series distribution. Because of the strong seasonality characterising Sicily’s rainfall regime, statistical analysis was separately applied to two data sets, referred to as “dry” and “wet” seasons, respectively. In this work, a similar analysis was carried out for a set of 26 DS time-series recorded in a large area (about 30000 km2), including Piedmont and the Aosta Valley. Area altitude ra…

rainfall dry spells polylogarithm-series distributionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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CONFRONTO TRA DATI DI TEMPERATURA RILEVATI IN AREE URBANE E IN AREE AGRICOLE LIMITROFE

2008

Il fenomeno noto come “isola di calore urbana” (Urban Heat Island, UHI), che riguarda prevalentemente i paesi più industrializzati, consiste nell’aumento della temperatura dell’aria nei centri abitati per effetto dell’urbanizzazione. La verifica di tale fenomeno è stata eseguita in Sicilia instaurando un confronto tra le temperature massime, minime e le escursioni termiche di coppie di stazioni di misura, poste rispettivamente all’interno e all’esterno di alcuni centri urbani minori nel periodo 2002-2005. L’analisi è stata sviluppata a scala annuale e semestrale (separando la stagione tipicamente secca, da Aprile a Settembre, da quella umida), in modo da rilevare in quali periodi dell’anno …

SiciliaUHIescursione termicapiccoli centri urbani
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A “Case Study” for the Estimation of Daily Solar Radiation from Measured Air Temperature Extremes in the Mid-Mediterranean Area

2012

Solar radiation Diurnal air temperature range Hargreaves‐Samani Bristow and Campbell Campbell and Donatelli Donatelli and BellocchiSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Agro-hydrological models to schedule irrigation of Mediterranean tree crops

2010

In this paper a comparison between two agro-hydrological models, used to schedule irrigation of typical Mediterranean tree crops, is assessed. In particular the comparison between the model proposed by FAO, using a black box processes schematization, and the SWAP model based on the numerical analysis of Richards’ equation is initially presented for two irrigation seasons, 2005 and 2006, and two Mediterranean tree crops, i.e. grapevine (Vitis vinifera, L.) and olive oil (Olea europea, L.). The comparison mainly focuses on hydrological balance components and on soil water contents. After investigating and setting the scheduling parameters ordinarily practiced by the framers in the area (i.e o…

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliAgrohydrological models FAO 56 SWAP Irrigation Scheduling Vineyard and Olive grove
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Stima della radiazione solare giornaliera in sicilia mediante i dati di temperatura massima e minima

2009

By using thermometric data series from 36 sicilian stations , the authors use different relationship for indirect determination of daily solar radiation. The best performance was given by Hargreaves-Samani formula which is then parameterized by the authors for the investigated region.

Daily solar radiation
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Un modello di generazione e trasporto del deflusso: Applicazione a un piccolo bacino

2005

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Tecnica scintillometrica per la misura dell’evapotraspirazione effettiva: principi teorici ed esempi applicativi

2009

evapotraspirazione micro-meteorologia scintillometro
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Assessing the agro hydrological SWAP model to simulate soil water balance in typical Mediterranean crops

2007

SOIL WATER BALANCE SWAP MODEL MEDITERRANEA CROPS
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Distribuzione di probabilità della portata di piena a scala di versante generata da deflusso hortoniano

2008

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestaliscala di versante deflusso hortoniano piena
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Gestione dell’irrigazione del vigneto attraverso l’uso di modelli di simulazione e misure di campo.

2008

In the paper the applicability of a numerical model, i.e. SWAP (Soil Water Atmosphere Plant), and a functional model, i.e. FAO 56, for irrigation scheduling is assessed. Model validation was initially carried out through the comparison between simulated and measured water content of a soil profile. The two models were then used in order to verify the possibility to simulate the typical irrigation management of the study area. In particular, the attitude of the two models to simulate the number and the distribution of watering, as well as the seasonal water consumption found in the ordinary management irrigation was assessed. Different scenarios of irrigation management allowed the analysis …

GESTIONE IRRIGAZIONE MODELLO SWAP MODELLO FAO-56Modello Agroidrologici FAO 56 SWAP Programmazione dell’Irrigazione del Vigneto.
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Trend of inter-arrival times of rainfall events for Italian Sub-Alpine and Mediterranean areas

2011

rainfall inter-arrival times Mediterranean environment sub-alpine environment discrete probability distributionSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Probability distribution of peak discharge at hillslope scale derived by an eco-hydrological approach

2006

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INDAGINE ECOIDROLOGICA SU UN VERSANTE CALANCHIVO IN SICILIA

2009

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestaliumidità del suolo bilancio idrologico ecoidrologia
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Determinazione del contenuto energetico delle precipitazioni tipiche dell'ambiente mediterraneo

2003

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalienergia cinetica della pioggiaerosione idrica da impatto
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Derivation of slope factor S of the USLE at basin scale by geomorphological approach

2007

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Sul tempo di risposta di un versante a prevalente deflusso hortoniano

2005

La distinzione del bacino idrografico in versanti e reticolo attiene ai differenti processi che in essi specificamente hanno luogo. In particolare i versanti sono sede dei fenomeni diffusi di formazione del deflusso superficiale e di erosione idrica, mentre la rete è sede dei fenomeni concentrati di trasporto del deflusso liquido e solido sino alla sezione di chiusura del bacino. Nell’ipotesi che la formazione prevalente del deflusso superficiale avvenga secondo lo schema hortoniano, tipico dei versanti privi di vegetazione, nel presente lavoro è suggerita una metodologia, applicabile anche ad altre modalità di formazione, per la valutazione del tempo caratteristico di risposta del versante…

risposta idrologica scala di versante formule applicativeSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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A model of dunnian flow at hillslope scale

2005

The development of a thin stream above the soil surface (overland flow) is associated to two mechanism of runoff generation on the hillslope: the infiltration excess (hortonian flow) and saturation excess (dunnian flow) mechanism. The first one is typical of arid and semi-arid regions, usually characterised by high rainfall intensities on soil exhibiting low permeability. The second one, firstly introduced by Hewlett and Hibbert, constitutes the main mechanism of runoff generation in humid regions, characterised by high groundwater table. In the last mechanism runoff is produced by contributing areas of restricted extent that expands with time, where near to the bottom of the hillslope a hi…

hillslope scale Hortonian and Dunnian flow Soil Saturation excessSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Applicability of a displaced-beam laser scintillometer in a sparse tall Mediterranean vegetation

2009

Recent studies showed that the sensible heat flux (H) measured with an array of eddy-correlation system has an high spatial and temporal variability over sparse tall vegetation, such as olive trees, whereas H determined with a displaced-beam laser scintillometer (DBLS) appeared to behave more stable. In this study, the results are shown of two field experiments performed over an olive tree plantation in Sicily in 2007 and 2008, in order to investigate the applicability of a DBSL in combination with remote sensing techniques for the actual evapotranspiration assessment. In 2007 the laser beams was closer to the top of the canopy than in 2008. Various aspects of the scintillation method will …

micro-meteorological measurements flux tower scintillometer sparse tall crop
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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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Coupling overland and subsurface flow model at hillslope scale

2008

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalioverland flow subsurface storm flow
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POSSIBILI MODIFICAZIONI DELLE COMPONENTI DEL BILANCIO IDROLOGICO INDOTTE DALLE VARIAZIONI CLIMATICHE

2008

ECOIDROLOGIASERIE TEMPORALISERIE DI UMIDITA' DEL SUOLO
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Primo contributo all'estensione di alcune serie climatiche siciliane mediante analisi di serie dendrocronologiche

2008

funzioni di rispostaSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestaliserie temporalidendroclimatologia
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Partitioning ET measurements for sparse vegetation: application to an olive orchard.

2011

continuum Soil-Plant-Atmosphere Actual Evapotranspiration Eddy covariance Sap Flow
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Modeling olive ecophysiological response to soil water deficit.

2011

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliOlive orchard water stress function sap flow Leaf water potential Irrigation
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