Search results for " water content"

showing 10 items of 77 documents

Diurnal Regulation of Leaf Water Status in High- and Low-Mannitol Olive Cultivars

2014

The role of mannitol and malic acid in the regulation of diurnal leaf water relations was investigated in ‘Biancolilla’ (high-mannitol) and ‘Cerasuola’ (low-mannitol) olive trees. Photosynthetic photon flux density (PPFD), vapor pressure deficit (VPD), stomatal conductance (gs), transpiration rate (T), relative water content (RWC), mannitol and malic acid were measured in ‘Biancolilla’ and ‘Cerasuola’ leaves during a dry and hot day of summer in Sicily. In general, leaves of ‘Biancolilla’ trees exhibited greater mannitol content, higher gs and T, but lower RWC than leaves of ‘Cerasuola’ trees. Differences in gs and T between the two cultivars were evident mainly in mid to late morning. ‘Bia…

Stomatal conductancemalate; polyol; relative water content; stomatal conductance; transpiration; vapor pressure deficitVapour Pressure DeficitPlant ScienceArticletranspirationchemistry.chemical_compoundmedicineCultivarWater contentEcology Evolution Behavior and SystematicsTranspirationmalateEcologyrelative water contentvapor pressure deficitBotanyOlive treesSettore AGR/03 - Arboricoltura Generale E Coltivazioni ArboreeHorticulturechemistrystomatal conductanceQK1-989polyolMannitolMalic acidmedicine.drugPlants; Volume 3; Issue 2; Pages: 196-208
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Effects of organic aerosol constituents on extinction and absorption coefficients and liquid water contents of fogs and clouds

1978

We have speculated on the influence of organic material on extinction and absorption coefficients and liquid water content of fogs and of clouds immediately after their condensational stage. It results therefore, that the reduction of the speed of growth from fog to cloud droplets due to the presence of organic films largely reduces the properties mentioned. Compared to that their increase coming from the surface tension reduction due to organic material being dissolved or building up films is expected to be less effective.

Surface tensionFogGeophysicsMaterials scienceGeochemistry and PetrologyThermodynamic equilibriumLiquid water contentExtinction (optical mineralogy)AbsorptanceAnalytical chemistryAbsorption (electromagnetic radiation)Atmospheric sciencesAerosolPure and Applied Geophysics PAGEOPH
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A semi-empirical approach for surface soil water content estimation from radar data without a-priori information on surface roughness

2006

Abstract In this study, the spatial distribution of soil water content in an agricultural area of 30 km 2 in Southern Italy has been estimated by using high-resolution space-borne Synthetic Aperture Radar data. Multi-polarised SAR images acquired during the SIR-C mission in April 1994 have been analysed by using the semi-empirical surface backscattering model derived by Oh, Y., Sarabandi K., Ulaby F.T., 1992. An empirical model and an inversion technique for radar scattering from bare soil surface. IEEE Trans. Geosci. Remote Sensing, 30(2), 370381. A site-specific calibration procedure of the cited model has been proposed to derive soil dielectric constant values without a-priori informatio…

Synthetic aperture radarHydrological modellingRadar backscatteringSurface finishSoil water contentlaw.inventionlawSoil waterSurface roughnessSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceSpatial variabilityHydrological modelRadarWater contentWater Science and TechnologyRemote sensingJournal of Hydrology
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Power sensitivity analysis of multi-frequency, multi-polarized, multi-temporal SAR data for soil-vegetation system variables characterization

2017

Abstract: The knowledge of spatial and temporal variability of soil water content and others soil-vegetation variables (leaf area index, fractional cover) assumes high importance in crop management. Where and when the cloudiness limits the use of optical and thermal remote sensing techniques, synthetic aperture radar (SAR) imagery has proven to have several advantages (cloud penetration, day/night acquisitions and high spatial resolution). However, measured backscattering is controlled by several factors including SAR configuration (acquisition geometry, frequency and polarization), and target dielectric and geometric properties. Thus, uncertainties arise about the more suitable configurati…

Synthetic aperture radarSpatial correlation010504 meteorology & atmospheric sciencesCloud coverScience0211 other engineering and technologies02 engineering and technologyBackscatteringSoil water content01 natural scienceslaw.inventionsensitivity analysislawSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalibackscattering; soil water content; surface roughness; leaf area index; sensitivity analysisRadarLeaf area indexWater content021101 geological & geomatics engineering0105 earth and related environmental sciencesRemote sensingSurface roughneQSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaSoil watersurface roughnessLeaf area indexSensitivity analysiBackscattering; Leaf area index; Sensitivity analysis; Soil water content; Surface roughness; Earth and Planetary Sciences (all)General Earth and Planetary SciencesEnvironmental scienceSpatial variabilityEarth and Planetary Sciences (all)Settore ICAR/06 - Topografia E Cartografia
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Nitrous oxide fluxes from permafrost regions

2020

This dataset is a synthesis of published nitrous oxide (N2O) fluxes from permafrost-affected soils in Arctic, Antarctic, and Alpine permafrost regions. The data includes mean N2O flux rates measured under field (in situ) conditions and in intact plant-soil systems (mesocosms) under near-field conditions. The dataset further includes explanatory environmental parameters such as meteorological data, soil physical-chemical properties, as well as site and experimental information. Data has been synthesized from published studies (see 'Further details'), and in some cases the authors of published studies have been contacted for additional site-level information. The dataset includes studies publ…

Temperature airNumber of pointsHemeroby/disturbanceannual meanNumber of measurement seasonsTemperature soilDensityArea localityPrecipitationgravimetricmeanNitrateTime in minutesAnalytical methodType of studyReference of dataTemperature air annual meanArea/localitypH soilCarbon Nitrogen ratioYear of observationWater holding capacityOriginal unitSample code/labelReplicatesNitrous oxidepHPermafrost extentThaw depth of active layer meanTemperatureMonthSample code labelZoneWater filled pore space calculatedExperimental treatmentCountryPrecipitation annual meanOrganic carbon soilEarth System ResearchSoil water content gravimetricType of chamberAmmoniumPresence/absenceNitrogenairvolumetricLocationactive layerType of disturbanceSiteVegetation typeWater filled pore spaceSoil water content volumetricSoil water contentin mass nitrous oxidesoilThaw depth of active layercalculatedbulkmaximumLONGITUDEOrganic carbonEcosystemPublication of dataPresence absenceSoil organic matterEvent labelThaw depth of active layer maximumNumber of measurementsHemeroby disturbanceNitrous oxide flux in mass nitrous oxideCarbon/Nitrogen ratiofluxOriginal valueLATITUDEDayNitrogen soilSoil moistureDensity active layer bulk
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Refractive index and equilibrium water content of conventional and silicone hydrogel contact lenses

2006

Prova tipográfica (In Press)

Traditional handheld refractometerMaterials scienceSiliconesRefractive index02 engineering and technologyRefraction Ocular03 medical and health scienceschemistry.chemical_compound0302 clinical medicineOpticsSiliconeRefractometerHumanssilicone hydrogelCLR 12-70Siloxane hydrogelScience & TechnologyEquilibrium water contentbusiness.industryWaterHydrogelsHEMAEquipment DesignContact Lenses Hydrophilic021001 nanoscience & nanotechnologyAtago N-2ESensory SystemsContact lensOphthalmologyRefractometrysoft contact lenschemistrySiloxaneSelf-healing hydrogels030221 ophthalmology & optometry0210 nano-technologybusinessRefractive indexRefractometryconventional hydrogelOptometryBiomedical engineering
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2014

Abstract. This study uses the EMAC atmospheric chemistry-climate model to simulate cloud properties and estimate cloud radiative effects induced by aerosols. We have tested two prognostic cloud droplet nucleation parameterizations, i.e., the standard STN (osmotic coefficient model) and hybrid (HYB, replacing the osmotic coefficient by the κ hygroscopicity parameter) schemes to calculate aerosol hygroscopicity and critical supersaturation, and consider aerosol–cloud feedbacks with a focus on warm clouds. Both prognostic schemes (STN and HYB) account for aerosol number, size and composition effects on droplet nucleation, and are tested in combination with two different cloud cover parameteriz…

TroposphereConvectionFogMeteorologyLiquid water contentChemistryCloud coverCloud albedoRadiative transferAtmospheric sciencesAerosolAtmospheric Chemistry and Physics Discussions
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Critical analysis of thermal inertia approaches for surface soil water content retrieval

2013

The “thermal inertia” method to retrieve surface soil water content maps on bare or sparsely-vegetated soils is analysed. The study area is a small experimental watershed, where optical and thermal images (in day and night time) and in situ data were simultaneously acquired. The sensitivity of thermal inertia to the phase difference between incoming radiation and soil temperature is demonstrated. Thus, to obtain an accurate value of the phase difference, the temporal distance between thermographs using a three-temperature approach is evaluated. We highlight when a cosine correction of the temperature needs to be applied, depending on whether the thermal inertia formulation includes two gene…

Watershedteneur en eau de la surface du soltélédétectionSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaRadiationthermal inertiasurface soil water contentremote sensinginertie thermiqueContent (measure theory)Soil waterThermalCalibrationEnvironmental scienceTrigonometric functionsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSensitivity (control systems)Settore ICAR/06 - Topografia E CartografiaWater Science and TechnologyRemote sensing
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Évolution du bilan hydrique à l'échelle de bassins versants en contexte de changement climatique – mise place d’une méthodologie

2014

Assessment of hydric balance at the catchment scale, under climate change scenario Face to climate change, public policies must implement adaptation strategies. This implies that the effects of climate change are plainly identified on territories. However, in the current state, data and knowledge at the local level are limited or not available to decision makers. This work proposes to well characterize the local impacts of climate change and to develop synergies between researchers and territorial actors to prepare the public decision.

[SDE] Environmental Scienceschangement climatiqueavailable water content[SDV]Life Sciences [q-bio]drainage dividemodelingbourgognebassin versant[SDV] Life Sciences [q-bio]water balanceclimate change[SDE]Environmental Sciences[SDV.BV]Life Sciences [q-bio]/Vegetal Biology[SDV.BV] Life Sciences [q-bio]/Vegetal Biologybilan hydriqueréserve utile en eauBurgundymodélisation
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Ultrathin Tropical Tropopause Clouds (UTTCs): II. Stabilization mechanisms

2003

Abstract. Mechanisms by which subvisible cirrus clouds (SVCs) might contribute to dehydration close to the tropical tropopause are not well understood. Recently Ultrathin Tropical Tropopause Clouds (UTTCs) with optical depths around 10-4 have been detected in the western Indian ocean. These clouds cover thousands of square kilometers as 200-300 m thick distinct and homogeneous layer just below the tropical tropopause. In their condensed phase UTTCs contain only 1-5% of the total water, and essentially no nitric acid. A new cloud stabilization mechanism is required to explain this small fraction of the condensed water content in the clouds and their small vertical thickness. This work sugges…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereAtmospheric ScienceSupersaturationWork (thermodynamics)010504 meteorology & atmospheric sciencesChemistry[SDU.OCEAN] Sciences of the Universe [physics]/Ocean AtmosphereEvaporationAtmospheric sciences010502 geochemistry & geophysics01 natural scienceslcsh:QC1-999lcsh:Chemistrylcsh:QD1-999Liquid water content13. Climate actionPhase (matter)Tropical tropopauseddc:550UpwellingCirruslcsh:Physics0105 earth and related environmental sciencesUTTCsultrathin tropical tropospause
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