Search results for "evapotranspiration"

showing 10 items of 183 documents

Mapping daily evapotranspiration at field to global scales using geostationary and polar orbiting satellite imagery

2010

Abstract. Thermal infrared (TIR) remote sensing of land-surface temperature (LST) provides valuable information about the sub-surface moisture status required for estimating evapotranspiration (ET) and detecting the onset and severity of drought. While empirical indices measuring anomalies in LST and vegetation amount (e.g., as quantified by the Normalized Difference Vegetation Index; NDVI) have demonstrated utility in monitoring ET and drought conditions over large areas, they may provide ambiguous results when other factors (soil moisture, advection, air temperature) are affecting plant stress. A more physically based interpretation of LST and NDVI and their relationship to sub-surface mo…

daily evapotranspirationglobal scalegeostationary satelliteSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Monitoring Water and Energy Cycles at Climate Scale in the Third Pole Environment (CLIMATE-TPE)

2021

A better understanding of the water and energy cycles at climate scale in the Third Pole Environment is essential for assessing and understanding the causes of changes in the cryosphere and hydrosphere in relation to changes of plateau atmosphere in the Asian monsoon system and for predicting the possible changes in water resources in South and East Asia. This paper reports the following results: (1) A platform of in situ observation stations is briefly described for quantifying the interactions in hydrosphere-pedosphere-atmosphere-cryosphere-biosphere over the Tibetan Plateau. (2) A multiyear in situ L-Band microwave radiometry of land surface processes is used to develop a new microwave r…

ddc:621.3Scienceearth observationAtmospheric sciencesevaporationTroposphereEvapotranspirationTibetan PlateauCryosphereEast Asian MonsoonmonsoonStratosphereThird Pole EnvironmentgeographyPlateaugeography.geographical_feature_categoryQITC-ISI-JOURNAL-ARTICLEGeneral Earth and Planetary SciencesEnvironmental scienceddc:620soil moistureITC-GOLDWater vaporThird Pole Environment; Tibetan Plateau; monsoon; earth observation; evaporation; soil moisture; microwave remote sensingHydrosphereRemote Sensing
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The use of shallow dripwater as an isotopic marker of seepage in karst areas: A comparison between Western Sicily (Italy) and the Harz Mountains (Ger…

2013

Abstract The isotopic signature of slow-flowing dripwater collected in caves located in Western Sicily (Italy) was determined for evaluating its possible use as an isotopic tracer of the local groundwater recharge. These spot measures were compared with a longer series of local rain and spring compositions and with other samples taken, under different hydrogeological conditions, in caves of the Harz Mountains (Northern Germany). The slow flowing dripwater from Sicily showed δ 18 O/δD ratios similar to those of local rain and groundwater, demonstrating that these three are all parent waters. A parallel similarity was found in the vertical isotopic gradient (Δδ 18 O) of the three groups of wa…

effective infiltration010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E Geomorfologiaevapotranspirationisotopic composition010502 geochemistry & geophysics01 natural sciencesIsotopic signatureCaveGeochemistry and PetrologyspringwatercaveEnvironmental Chemistryrain0105 earth and related environmental sciencesHydrologygeographyHydrogeologygeography.geographical_feature_categorydripwaterGroundwater rechargeKarstPollution6. Clean waterSettore GEO/08 - Geochimica E VulcanologiaWater resourcesInfiltration (hydrology)GeologyGroundwaterApplied Geochemistry
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Application of energy balance models for actual evapotranspiration assessment by means of airborne and satellite remote sensing data

2008

evapotranspiration remote sensing energy balance
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Effects of morphology on watershed actual evapotranspiration estimation by means of SEBAL model

2008

evapotranspiration remote sensing morphology watershed
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Comparative analysis of surface energy balance models for actual evapotranspiration estimation through remotely sensed images

2012

evapotranspiration remote sensing surface energy balanceSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Pampa Biome Environmental Particularities Regarding to Energy Balance

2020

Ecosystem evapotranspiration (ET) has been quantified around the world by different methodologies to understand the energy balance, especially to control the evolution of climate change. It is known that the vegetation of the pampa biome is natural grasslands, it has a large variety of species (flora and fauna), however is it different in the environmental aspects related to the energy balance when compared to the grassland cultivated? In this study the objective was to analyze the environmental differences of the Pampa Biome related to the energy balance in comparison with the pastures cultivated in Barrax, Spain. In the first one the minimum daily ET is 0.99 mm/day, while in the second is…

geographygeography.geographical_feature_categoryEvapotranspirationBiomeEnergy balanceEnvironmental scienceClimate changeEcosystemPhysical geographyVegetationGrasslandNormalized Difference Vegetation Index2020 IEEE Latin American GRSS & ISPRS Remote Sensing Conference (LAGIRS)
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Simple soil water balance model (R function)

2022

This R function models the soil water balance (SWB) for two soil layers based on relatively simple assumptions. It is a simple method to calculate actual evapotranspiration, downward water flux (leaching), and upward water flux (or capillary rise) from two soil layers and the net flux between the two soil layers. The necessary input data comprises the change in soil water storage between two time steps per soil layer (e.g. from repeated volumetric soil water content measurements), potential evapotranspiration, precipitation, and the percentage of roots in the top soil layer. The soil water balance model is described in detail in Leimer et al. (2014). It is based on a soil water balance mode…

https://w3id.org/skgo/modsci#SoilScienceevapotranspirationRhttps://w3id.org/skgo/modsci#Hydrologywater flux
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Indo-French High-resolution Thermal Infrared Space Mission for Earth Natural Resources Assessment and Monitoring -Concept and Definition of TRISHNA

2019

The Indian and French Space Agencies, ISRO and CNES, have conceptualized a space-borne Thermal Infrared Reflectance (TIR) mission, TRISHNA (Thermal infRared Imaging Satellite for High-resolution Natural Resource Assessment). The primary design drivers of TRISHNA are the monitoring of (i) terrestrial water stress and use, and of (ii) coastal and continental water. A suit of four TIR bands and six optical bands is planned. The TIR bands will be centred at 8.6 μm, 9.1 μm, 10.3 μm and 11.5 μm to provide noon-night global observations at 57m nadir resolution over land and coastal regions. The field of view (FOV) is ±34° and the orbit of 761&thin…

lcsh:Applied optics. Photonics010504 meteorology & atmospheric sciences0207 environmental engineering[SDU.STU]Sciences of the Universe [physics]/Earth Sciences02 engineering and technology01 natural scienceslcsh:Technologyglobal monitoringEvapotranspirationNadir020701 environmental engineering0105 earth and related environmental sciencesRemote sensingTIR remote sensing;surface energy balance;TRISHNA mission;global monitoringSpacecraftbusiness.industrylcsh:Tsurface energy balancePrimary productionlcsh:TA1501-1820Natural resourceTRISHNA mission13. Climate actionlcsh:TA1-2040TIR remote sensingEnvironmental scienceRadiometrySatellitebusinesslcsh:Engineering (General). Civil engineering (General)Water use
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Mapping daily evapotranspiration at field to continental scales using geostationary and polar orbiting satellite imagery

2011

Abstract. Thermal infrared (TIR) remote sensing of land-surface temperature (LST) provides valuable information about the sub-surface moisture status required for estimating evapotranspiration (ET) and detecting the onset and severity of drought. While empirical indices measuring anomalies in LST and vegetation amount (e.g., as quantified by the Normalized Difference Vegetation Index; NDVI) have demonstrated utility in monitoring ET and drought conditions over large areas, they may provide ambiguous results when other factors (e.g., air temperature, advection) are affecting plant functioning. A more physically based interpretation of LST and NDVI and their relationship to sub-surface moistu…

lcsh:GE1-350Meteorologylcsh:TPlanetary boundary layerSettore ICAR/02 - Costruzioni Idrauliche E Marittime E Idrologialcsh:Geography. Anthropology. RecreationPolar orbitVegetationlcsh:Technologyremote sensing mapping ET ALEXIlcsh:TD1-1066Normalized Difference Vegetation Indexlcsh:GEvapotranspirationGeostationary orbitEnvironmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSatelliteSatellite imagerylcsh:Environmental technology. Sanitary engineeringlcsh:Environmental sciencesRemote sensing
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