Search results for "PET"

showing 10 items of 12749 documents

Developments for vegetation fluorescence retrieval from spaceborne high-resolution spectrometry in the O2-A and O2-B absorption bands

2010

Solar-induced chlorophyll fluorescence is a weak electromagnetic signal emitted in the red and far-red spectral regions by vegetation chlorophyll under excitation by solar radiation. Chlorophyll fluorescence has been demonstrated to be a close proxy to vegetation physiological functioning. The basis for fluorescence retrieval from passive space measurements is the exploitation of the O2-A and O2-B atmospheric absorption features to isolate the fluorescence signal from the solar radiation reflected by the surface and the atmosphere. High spectral resolution measurements and a precise modeling of the atmospheric radiative transfer in the visible and near-infrared regions are mandatory. Recent…

Atmospheric ScienceSoil ScienceAquatic ScienceRadiationOceanographychemistry.chemical_compoundOpticsGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Radiative transferSpectral resolutionSpectroscopyChlorophyll fluorescenceEarth-Surface ProcessesWater Science and TechnologyRemote sensingEcologybusiness.industryPaleontologyForestryFluorescenceGeophysicschemistrySpace and Planetary ScienceAbsorption bandChlorophyllEnvironmental sciencebusinessJournal of Geophysical Research
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Performance of DEMETER calibration for rainfall forecasting purposes: Application to the July–August Sahelian rainfall

2008

International audience; This work assesses and compares the skill of direct and model-output-statistics (MOS) calibrated hindcasts of the July–August rainfall amounts for the dry period 1980–2000 over the Sahel issued from the Development of a European Multimodel Ensemble System for Seasonal to Interannual Prediction (DEMETER) experiment, with the aim to highlight among the simulated parameters, i.e., those potentially relevant for rainfall forecasts purposes. Three approaches were used: the DEMETER (1) direct rainfall, (2) MOS-calibrated rainfall, and (3) MOS-calibrated atmospheric dynamics and energy. Canonical correlation analyses (CCA) were employed in the two latter approaches to calib…

Atmospheric ScienceSoil ScienceForecast skillAquatic ScienceOceanographyMonsoonMediterranean seaGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Moist static energyHindcastEarth-Surface ProcessesWater Science and Technologycanonical correlation analysisEcologyMode (statistics)PaleontologyForestryAfrican easterly jet[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsmodel output statistics approachSpace and Planetary ScienceClimatologyEnvironmental science[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatologyseasonal rainfall forecasts in West Africacanonical correlation analysis.Teleconnection
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A solar storm observed from the Sun to Venus using the STEREO, Venus Express, and MESSENGER spacecraft

2009

The suite of SECCHI optical imaging instruments on the STEREO-A spacecraft is used to track a solar storm, consisting of several coronal mass ejections (CMEs) and other coronal loops, as it propagates from the Sun into the heliosphere during May 2007. The 3-D propagation path of the largest interplanetary CME (ICME) is determined from the observations made by the SECCHI Heliospheric Imager (HI) on STEREO-A (HI-1/2A). Two parts of the CME are tracked through the SECCHI images, a bright loop and a V-shaped feature located at the rear of the event. We show that these two structures could be the result of line-of-sight integration of the light scattered by electrons located on a single flux rop…

Atmospheric ScienceSoil ScienceInterplanetary mediumVenusAquatic ScienceSpace weatherOceanographyGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Coronal mass ejectionAstrophysics::Solar and Stellar AstrophysicsEarth-Surface ProcessesWater Science and TechnologyPhysicsEcologybiologyPaleontologyAstronomyForestryCoronal loopbiology.organism_classificationSolar windGeophysicsSpace and Planetary SciencePhysics::Space PhysicsInterplanetary spaceflightHeliosphereJournal of Geophysical Research: Space Physics
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Ice nucleation properties of the most abundant mineral dust phases

2008

[1] The ice nucleation properties of the nine most abundant minerals occurring in desert aerosols (quartz, albite, microcline, kaolinite, montmorillonite, illite, calcite, gypsum, and hematite) were investigated by environmental scanning electron microscopy (ESEM). In this instrument, the pure minerals are exposed to water vapor at variable pressures and temperatures. The crystallization of ice on the mineral particles is observed by secondary electron imaging, and the supersaturation for an activated particle fraction of 1–3% is determined as function of temperature. In all experiments, condensation of water prior to ice formation was not observed within detectable limits, even at water su…

Atmospheric ScienceSoil ScienceMineralogyAquatic ScienceMineral dustengineering.materialOceanographychemistry.chemical_compoundAlbiteGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)KaoliniteRelative humidityEarth-Surface ProcessesWater Science and TechnologyCalciteSupersaturationEcologyPaleontologyForestryGeophysicschemistrySpace and Planetary ScienceIlliteIce nucleusengineeringGeologyJournal of Geophysical Research
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Optical properties of deep glacial ice at the South Pole

2006

We have remotely mapped optical scattering and absorption in glacial ice at the South Pole for wavelengths between 313 and 560 nm and depths between 1100 and 2350 m. We used pulsed and continuous light sources embedded with the AMANDA neutrino telescope, an array of more than six hundred photomultiplier tubes buried deep in the ice. At depths greater than 1300 m, both the scattering coefficient and absorptivity follow vertical variations in concentration of dust impurities, which are seen in ice cores from other Antarctic sites and which track climatological changes. The scattering coefficient varies by a factor of seven, and absorptivity (for wavelengths less than ∼450 nm) varies by a fact…

Atmospheric ScienceSoil ScienceMineralogyAquatic ScienceOceanographyLight scatteringPhysics::GeophysicsIce coreGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Absorption (electromagnetic radiation)Physics::Atmospheric and Oceanic PhysicsEarth-Surface ProcessesWater Science and Technologygeographygeography.geographical_feature_categoryEcologyScatteringPaleontologyForestryGlacierMolar absorptivityWavelengthGeophysicsSpace and Planetary ScienceAttenuation coefficientAstrophysics::Earth and Planetary AstrophysicsGeologyJournal of Geophysical Research
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Geogenic and atmospheric sources for volatile organic compounds in fumarolic emissions from Mt. Etna and Vulcano Island (Sicily, Italy)

2012

[1] In this paper, fluid source(s) and processes controlling the chemical composition of volatile organic compounds (VOCs) in gas discharges from Mt. Etna and Vulcano Island (Sicily, Italy) were investigated. The main composition of the Etnean and Volcano gas emissions is produced by mixing, to various degrees, of magmatic and hydrothermal components. VOCs are dominated by alkanes, alkenes and aromatics, with minor, though significant, concentrations of O-, S- and Cl(F)-substituted compounds. The main mechanism for the production of alkanes is likely related to pyrolysis of organic-matter-bearing sediments that interact with the ascending magmatic fluids. Alkanes are then converted to alken…

Atmospheric ScienceSoil ScienceMineralogyAquatic ScienceOceanographyMethaneHydrothermal circulationchemistry.chemical_compoundGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Chemical compositionEarth-Surface ProcessesWater Science and Technologychemistry.chemical_classificationgeographygeography.geographical_feature_categoryEcologyAlkenePaleontologyForestryFumaroleAbiogenic petroleum originGeophysicschemistryVolcanoSpace and Planetary ScienceEnvironmental chemistryPyrolysisGeologyJournal of Geophysical Research: Atmospheres
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Variation of H2O/CO2and CO2/SO2ratios of volcanic gases discharged by continuous degassing of Mount Etna volcano, Italy

2008

[1] We applied the Multi-GAS technique to measure compositions of the volcanic plumes continuously discharged from summit craters of Voragine, Northeast and Bocca Nuova at Mount Etna, in an attempt to estimate compositions of the source volcanic gases. The estimated CO2/SO2 and H2O/CO2 ratios of the volcanic gases show a large variation ranging from 0.6 to 30 and from 1 to 18, respectively. This variability overlaps with the compositional range of dissolved volatiles in melt inclusions and their coexisting bubbles in a magma chamber and can be caused by the low-pressure degassing of a magma with variable bubble content ranging from 0.3 to 15 wt.%. The variable bubble content in the magma is…

Atmospheric ScienceSoil ScienceMineralogyMagma chamberAquatic ScienceOceanographyVolcanic GasesImpact craterGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)eventGas compositionPetrologyEarth-Surface ProcessesWater Science and TechnologyMelt inclusionsevent.disaster_typegeographygeography.geographical_feature_categoryEcologyPaleontologyForestryGeophysicsVolcanoSpace and Planetary ScienceMagmaGeologyVolcanic ashJournal of Geophysical Research
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Overview of the magnetic properties experiments on the Mars Explorations Rovers

2009

[1] The Mars Exploration Rovers have accumulated airborne dust on different types of permanent magnets. Images of these magnets document the dynamics of dust capture and removal over time. The strongly magnetic subset of airborne dust appears dark brown to black in Panoramic Camera (Pancam) images, while the weakly magnetic one is bright red. Images returned by the Microscopic Imager reveal the formation of magnetic chains diagnostic of magnetite-rich grains with substantial magnetization (>8 Am2 kg−1). On the basis of Mossbauer spectra the dust contains magnetite, olivine, pyroxene, and nanophase oxides in varying proportions, depending on wind regime and landing site. The dust contains a …

Atmospheric ScienceSoil ScienceMineralogyPyroxeneAquatic Scienceengineering.materialOceanographychemistry.chemical_compoundMagnetizationGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Earth-Surface ProcessesWater Science and TechnologyMagnetiteBasaltOlivineEcologySpinelPaleontologyForestryMars Exploration Programequipment and suppliesSilicateGeophysicschemistrySpace and Planetary ScienceengineeringGeology
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A numerical study of atmospheric signals in the Earth-ionosphere electromagnetic cavity with the Transmission Line Matrix method

2006

[1] The effect of the Earth-ionosphere electromagnetic cavity on the spectrum of an atmospheric signal generated by a broadband electrical current source is analyzed numerically by means of the Transmission Line Matrix (TLM) method. Two new TLM meshes are developed, one with transmission lines connected in parallel and the other with connections in series. The equations describing propagation through these parallel or series meshes are equivalent to the Maxwell equations for TEr or TMr modes in the spherical Earth-ionosphere cavity, respectively. The numerical algorithm obtains Schumann resonance frequencies very close to the experimental ones, confirming that this methodology is a valid nu…

Atmospheric ScienceSoil ScienceTransmission-line matrix methodAquatic ScienceOceanographysymbols.namesakeOpticsGeochemistry and PetrologyTransmission lineElectromagnetic cavityEarth and Planetary Sciences (miscellaneous)Earth-Surface ProcessesWater Science and TechnologyPhysicsEcologySchumann resonancesbusiness.industryPaleontologyResonanceForestryComputational physicsGeophysicsMaxwell's equationsSpace and Planetary SciencesymbolsIonospherebusinessMatrix methodJournal of Geophysical Research
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Crustal dynamics of Mount Vesuvius from 1998 to 2005: Effects on seismicity and fluid circulation

2008

[1] This paper presents the results of hydrogeochemical and seismological studies carried out at Mount Vesuvius during the period June 1998 to December 2005. Hydrogeochemical data show the occurrence of slowly varying long-term variations in the total dissolved salts and bicarbonate contents of the groundwaters, accompanied by a general decline in water temperatures. The temporal distributions of air temperature and rainfall in the Vesuvius area suggest that these variations do not depend on changes in the hydrological regime. The changes in the geochemical parameters are accompanied by slight variations in both the seismicity rate and energy release. A further relationship between seismic …

Atmospheric ScienceSoil Sciencehydrogeochemistry vesuviusAquiferAquatic ScienceInduced seismicityOceanographyGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Earth-Surface ProcessesWater Science and Technologygeographygeography.geographical_feature_categoryEcologyPaleontologyForestryAtmospheric temperatureStress fieldGeophysicsVolcanoShear (geology)Space and Planetary ScienceSedimentary rockGroundwaterGeologySeismologyJournal of Geophysical Research
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