Search results for " EXTREME EVENTS"

showing 7 items of 7 documents

Establishing a soil loss threshold for limiting rilling

2015

In this paper a frequency analysis of event soil loss measurements collected in the period 1999–2012 at the microplots and plots of the Sparacia Experimental Area in Sicily, southern Italy, was developed. The analysis was carried out using the annual maximum soil loss measurements normalized by the mean soil loss measured at a given temporal and spatial scale. The empirical frequency distribution of the normalized variable was well fitted by two Gumbel’s theoretical probability distributions discriminated by a value of the normalized variable equal to 2. This last value discriminates between the relatively low and frequent values of the normalized variable and the high and rare ones. The an…

HydrologySoil loss toleranceFrequency analysisScale (ratio)Soil erosion measurements Probability distributions Extreme events Soil loss tolerance RillingSoil scienceLimitinglaw.inventionSoil lossGumbel distributionlawSpatial ecologyEnvironmental ChemistryEnvironmental scienceProbability distributionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeneral Environmental ScienceWater Science and TechnologyCivil and Structural Engineering
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The geo-hydrologic event in the Peloritan – Ionian area of 2009: debris-flow susceptibility assessment by means of forward logistic regression

2012

On the 1st of October 2009, the area centred on the village of Giampilieri (Messina), on the Ionian side of the Peloritan belt, suffered thousands of landslides activated in the time lapse of about five hours, which caused 36 victims, more than 100 injured and more than 0.5M€ of damage to structures. This unprecedented phenomenon was triggered by an exceptional meteorological event, recorded at the foothills with 250mm of rain in just 8 hours; this amount of rainfall was cumulated to two previous events (16/IX: 75mm; 23/IX: 190mm) for a total amount of more than 500mm in less than two weeks. Due to the peculiar triggering conditions a huge number of debris flows involved the shallow weather…

Settore GEO/04 - Geografia Fisica E Geomorfologiasusceptibility logistic regression EXTREME EVENTS
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Statistical distribution of soil loss and sediment yield at Sparacia experimental area, Sicily

2010

Abstract An analysis of the statistical distribution of event soil loss was carried out using the data collected in the period 1999–2008 at the microplots and plots of the Sparacia experimental area (Sicily, Italy). For a given microplot size, the analysis allowed to establish that the soil loss frequency distribution was skewed. Using the soil loss normalized by the event mean value, the analysis also showed that the frequency distributions corresponding to different microplot and plot sizes were overlapping, i.e. all distributions were extracted by the same statistical population. The developed analysis allowed to suggest that the soil loss of a given return period can be estimated using …

HydrologyReturn periodSoil erosion sediment yield measurements probability distributions extreme eventsStatistical populationErosionSedimentEnvironmental scienceProbability distributionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSpatial variabilityStructural basinFrequency distributionEarth-Surface Processes
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Study of the effects of climate extremes on functioning of intertidal assemblages to design an early warning sensor network

2020

Settore BIO/07 - Ecologiaclimate extreme events metabolismecosystem functioning macroalgae early warning signals intertidal
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Projecting Exposure to Extreme Climate Impact Events Across Six Event Categories and Three Spatial Scales

2020

Summarization: The extent and impact of climate‐related extreme events depend on the underlying meteorological, hydrological, or climatological drivers as well as on human factors such as land use or population density. Here we quantify the pure effect of historical and future climate change on the exposure of land and population to extreme climate impact events using an unprecedentedly large ensemble of harmonized climate impact simulations from the Inter‐Sectoral Impact Model Intercomparison Project phase 2b. Our results indicate that global warming has already more than doubled both the global land area and the global population annually exposed to all six categories of extreme events co…

010504 meteorology & atmospheric sciencesHYDROLOGICAL MODELSPopulation0207 environmental engineeringFLOOD RISKEnvironmental Sciences & Ecology02 engineering and technologySubtropics[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology01 natural sciencesPopulation densityLatitudeClimate-related extreme events/dk/atira/pure/sustainabledevelopmentgoals/climate_actionEarth and Planetary Sciences (miscellaneous)SDG 13 - Climate ActionMeteorology & Atmospheric SciencesBURNED AREAGLOBAL CROP PRODUCTIONGeosciences Multidisciplinary020701 environmental engineeringeducation0105 earth and related environmental sciencesGeneral Environmental ScienceEvent (probability theory)education.field_of_studyScience & TechnologyLand useGlobal warmingGlobal warmingVEGETATION MODEL ORCHIDEEGeology15. Life on landTERRESTRIAL CARBON BALANCE13. Climate actionClimatologyPhysical SciencesTROPICAL CYCLONE ACTIVITYHURRICANE INTENSITYEnvironmental scienceTropical cycloneINTERANNUAL VARIABILITYLife Sciences & BiomedicineEnvironmental SciencesINCORPORATING SPITFIRE
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Evapotranspiration simulations in ISIMIP2a-Evaluation of spatio-temporal characteristics with a comprehensive ensemble of independent datasets

2018

Actual land evapotranspiration (ET) is a key component of the global hydrological cycle and anessential variable determining the evolution of hydrological extreme events under different climate change scenarios. However, recently available ET products show persistent uncertainties thatare impeding a precise attribution of human-induced climate change. Here, we aim at comparing arange of independent global monthly land ET estimates with historical model simulations from theglobal water, agriculture, and biomes sectors participating in the second phase of the Inter-SectoralImpact Model Intercomparison Project (ISIMIP2a). Among the independent estimates, we use theEartH2Observe Tier-1 dataset …

PARAMETERIZATION010504 meteorology & atmospheric sciences0208 environmental biotechnologyREANALYSIS DATA02 engineering and technologyForcing (mathematics)01 natural sciencesISIMIP2aEnvironmental Science(all)Evapotranspirationddc:550Range (statistics)Cluster AnalysisMeteorology & Atmospheric SciencesWATERWater cycleuncertaintyGeneral Environmental ScienceUncertaintyVariance (accounting)Explained variationGLOBAL TERRESTRIAL EVAPOTRANSPIRATIONVariable (computer science)[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyPhysical SciencesLife Sciences & BiomedicinePROJECTHYDROLOGICAL MODELSevapotranspirationClimate changeEnvironmental Sciences & EcologySOIL-MOISTUREhydrological extreme eventsLAND-SURFACE MODELhydrological extreme events ; cluster analysis ; uncertainty ; ISIMIP2a ; evapotranspiration[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/HydrologyHydrological extreme events0105 earth and related environmental sciencesScience & TechnologyRenewable Energy Sustainability and the EnvironmentPublic Health Environmental and Occupational HealthPOTENTIAL EVAPOTRANSPIRATION020801 environmental engineeringEarth sciencesISIMIP2a; evapotranspiration; uncertainty; cluster analysis; hydrological extreme events13. Climate actionEnvironmental scienceEnvironmental SciencesHIGH-RESOLUTIONcluster analysis
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Long-Term Climate Trends and Extreme Events in Northern Fennoscandia (1914–2013)

2017

We studied climate trends and the occurrence of rare and extreme temperature and precipitation events in northern Fennoscandia in 1914–2013. Weather data were derived from nine observation stations located in Finland, Norway, Sweden and Russia. The results showed that spring and autumn temperatures and to a lesser extent summer temperatures increased significantly in the study region, the observed changes being the greatest for daily minimum temperatures. The number of frost days declined both in spring and autumn. Rarely cold winter, spring, summer and autumn seasons had a low occurrence and rarely warm spring and autumn seasons a high occurrence during the last 20-year interval (1994–2013…

0106 biological sciencesextreme eventsAtmospheric Science010504 meteorology & atmospheric sciencesclimate trends climate warming cold season extreme events northern Fennoscandiata1171010603 evolutionary biology01 natural sciencesExtreme temperatureclimate warmingSpring (hydrology)Precipitationsääilmiötlcsh:Science0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorycold seasonCold seasonGlobal warmingExtreme eventsilmastonmuutoksetclimate trendsnorthern Fennoscandiasademäärä13. Climate actionClimatologyFennoskandiaFrostPeriod (geology)Environmental sciencelämpötilalcsh:QClimate
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