Search results for "forestry"

showing 10 items of 1998 documents

Rates of carbon dioxide plume degassing from Mount Etna volcano,

2006

We report here on the real-time measurement of CO2 and SO2 concentrations in the near-vent volcanic gas plume of Mount Etna, acquired by the use of a field portable gas analyzer during a series of periodic field surveys on the volcano's summit. During the investigated period (September 2004 to September 2005), the plume CO2/SO2 ratio ranged from 1.9 to 10.8, with contrasting composition for Northeast and Voragine crater plumes. Scaling the above CO2/SO2 ratios by UV spectroscopy determined SO2 emission rates, we estimate CO2 emission rates from the volcano in the range 0.9-67.5 kt d-1 (average, 9 kt d-1). About 2 kt of CO2 were emitted daily on average during quiescent passive degassing, wh…

Atmospheric ScienceVolcanic hazardsSoil ScienceMineralogyAquatic ScienceOceanographyAtmospheric scienceschemistry.chemical_compoundImpact craterGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)PanacheEarth-Surface ProcessesWater Science and Technologygeographygeography.geographical_feature_categoryEcologyPaleontologyForestryGas analyzerPlumeGeophysicsVolcanochemistrySpace and Planetary ScienceMagmaCarbon dioxideEtnaCO2Geology
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Foam effect on the sea surface emissivity in the 8–14μm region

2007

[1] The effect of foam on the sea surface emission has been studied in the microwave region, but its effect on thermal infrared emissivity and temperature has not been sufficiently analyzed in the literature. This paper presents thermal infrared measurements of foam-covered seawaters carried out under controlled conditions using a multichannel radiometer working in the 8–14 μm region. The experimental data show a negligible foam effect at low observation angles but a significant increase of emissivity with foam at angles above 45°. Differences between foam and foam-free emissivities are about +0.04 for observation angles of 65°, depending slightly on the radiometric spectral band. The effec…

Atmospheric ScienceYield (engineering)RadiometerMaterials scienceEcologyPaleontologySoil ScienceMineralogyForestrySpectral bandsAquatic ScienceOceanographySea surface temperatureGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)EmissivitySatelliteSeawaterMicrowaveEarth-Surface ProcessesWater Science and TechnologyRemote sensingJournal of Geophysical Research
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Composition and diurnal variability of the natural Amazonian aerosol

2003

As part of the Large-Scale Biosphere-Atmosphere Experiment in Amazonia (LBA)-Cooperative LBA Airborne Regional Experiment (CLAIRE) 2001 campaign, separate day and nighttime aerosol samples were collected in July 2001 at a ground-based site in Amazonia, Brazil, in order to examine the composition and temporal variability of the natural “background” aerosol. A combination of analytical techniques was used to characterize the elemental and ionic composition of the aerosol. Major particle types larger than ∼0.5 μm were identified by electron and light microscopy. Both the coarse and fine aerosol were found to consist primarily of organic matter (∼70 and 80% by mass, respectively), with the coar…

Atmospheric Sciencefood.ingredientSoil ScienceMineralogyAquatic ScienceOceanographychemistry.chemical_compoundfoodGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Organic matterSulfateEarth-Surface ProcessesWater Science and Technologychemistry.chemical_classificationTotal organic carbonEcologySea saltPaleontologyForestryParticulatesAerosolGeophysicschemistrySpace and Planetary ScienceEnvironmental chemistryParticleBioaerosolJournal of Geophysical Research: Atmospheres
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Gas emission strength and evolution of the molar ratio of BrO/SO2 in the plume of Nyiragongo in comparison to Etna

2015

Airborne and ground-based differential optical absorption spectroscopy observations have been carried out at the volcano Nyiragongo (Democratic Republic of Congo) to measure SO2 and bromine monoxide (BrO) in the plume in March 2004 and June 2007, respectively. Additionally filter pack and multicomponent gas analyzer system (Multi-GAS) measurements were carried out in June 2007. Our measurements provide valuable information on the chemical composition of the volcanic plume emitted from the lava lake of Nyiragongo. The main interest of this study has been to investigate for the first time the bromine emission flux of Nyiragongo (a rift volcano) and the BrO formation in its volcanic plume. Mea…

Atmospheric Sciencegas emissionEcologybromineSoil SciencePaleontologyForestryAquatic ScienceOceanographyFlussiNyiragongoGeochemistry and PetrologySpace and Planetary ScienceEarth-Surface ProcesseEarth and Planetary Sciences (miscellaneous)BromoGeophysicWater Science and Technology
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Hurricane Impact on Seepage Water in Larga Cave, Puerto Rico

2018

Atmospheric Sciencegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesEcologyPaleontologySoil ScienceForestryAquatic Science010502 geochemistry & geophysics01 natural sciencesPaleotempestologyOceanographyCavePaleoclimatologyEnvironmental scienceTropical cyclone0105 earth and related environmental sciencesWater Science and TechnologyJournal of Geophysical Research: Biogeosciences
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Reactive halogen chemistry in volcanic plumes

2007

[1] Bromine monoxide (BrO) and sulphur dioxide (SO2) abundances as a function of the distance from the source were measured by ground-based scattered light Multiaxis Differential Optical Absorption Spectroscopy (MAX-DOAS) in the volcanic plumes of Mt. Etna on Sicily, Italy, in August–October 2004 and May 2005 and Villarica in Chile in November 2004. BrO and SO2 spatial distributions in a cross section of Mt. Etna's plume were also determined by Imaging DOAS. We observed an increase in the BrO/SO2 ratio in the plume from below the detection limit near the vent to about 4.5 × 10−4 at 19 km (Mt. Etna) and to about 1.3 × 10−4 at 3 km (Villarica) distance, respectively. Additional attempts were …

Atmospheric Sciencegeographygeography.geographical_feature_categoryEcologyAbsorption spectroscopyThermodynamic equilibriumDifferential optical absorption spectroscopyPaleontologySoil ScienceMineralogyForestryAquatic ScienceOceanographySpatial distributionPlumeBrOGeophysicsVolcanoSpace and Planetary ScienceGeochemistry and PetrologyHalogenEarth and Planetary Sciences (miscellaneous)PanacheEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Volcanic plume monitoring at Mount Etna by diffusive (passive) sampling

2004

[1] This paper reports the use of diffusive tubes in determining HF, HCl, and SO2 in the volcanic plume of Mount Etna in an attempt to highlight the potential of this method in studying volcanoes. In a first application a network of 18 diffusive tubes was installed on Etna's flanks, aimed at evaluating the atmospheric dispersion of the volcanic plume on a local scale. Results showed a monotonic decrease in volatile air concentrations with distance from the craters (HF from 0.15 to <0.003 μmol m−3, HCl from 2 to <0.01 μmol m−3, and SO2 from 11 to 0.04 μmol m−3), revealing the prevalently volcanic contribution. Matching of SO2/HCl and HCl/HF volatile ratios with contemporaneous measurements a…

Atmospheric Sciencegeographygeography.geographical_feature_categoryEcologyPaleontologySoil ScienceMineralogyForestryAquatic ScienceAtmospheric dispersion modelingOceanographyPlumeGeophysicsVolcanoImpact craterVolcanic plumeSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)PanacheChemical compositionGeologyEarth-Surface ProcessesWater Science and TechnologyPassive samplingJournal of Geophysical Research: Atmospheres
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Sources, size distribution, and downwind grounding of aerosols from Mount Etna

2006

The number concentrations and size distributions of aerosol particles >0.3 mm diameter were measured at the summit of Mount Etna and up to 10 km downwind from the degassing vents during July and August 2004. Aerosol number concentrations reached in excess of 9 106 L1 at summit vents, compared to 4–8 104 L1 in background air. Number concentrations of intermediate size particles were higher in emissions from the Northeast crater compared to other summit crater vents, and chemical composition measurements showed that Northeast crater aerosols contained a higher mineral cation content compared to those from Voragine or Bocca Nuova, attributed to Strombolian or gas puffing activity within the ve…

Atmospheric Sciencegeographygeography.geographical_feature_categoryEcologyParticle numberPaleontologySoil ScienceMineralogyForestryAquatic ScienceOceanographyStrombolian eruptionPlumeAerosolGeophysicsImpact craterVolcanoSpace and Planetary ScienceGeochemistry and PetrologyParticle-size distributionEarth and Planetary Sciences (miscellaneous)PanacheEnvironmental scienceEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research: Atmospheres
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Spirit Mars Rover Mission to the Columbia Hills, Gusev Crater: Mission overview and selected results from the Cumberland Ridge to Home Plate

2008

This paper summarizes the Spirit rover operations in the Columbia Hills of Gusev Crater from sols 513 to 1476 and provides an overview of selected findings that focus on synergistic use of the Athena Payload and comparisons to orbital data. Results include discovery of outcrops (Voltaire) on Husband Hill that are interpreted to be altered impact melt deposits that incorporated local materials during emplacement. Evidence for extensive volcanic activity and aqueous alteration in the Inner Basin is also detailed, including discovery and characterization of accretionary lapilli and formation of sulfate, silica, and hematite-rich deposits. Use of Spirit's data to understand the range of spectra…

Atmospheric Sciencegeographygeography.geographical_feature_categoryEcologyWater on MarsPaleontologySoil ScienceForestryMars Exploration ProgramAquatic ScienceOceanographyExploration of MarsCRISMAstrobiologyMars roverGeophysicsVolcanoImpact craterSpace and Planetary ScienceGeochemistry and PetrologyRidgeEarth and Planetary Sciences (miscellaneous)GeologyEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Modeling suggests that oblique extension facilitates rifting and continental break-up

2012

[1] In many cases the initial stage of continental break-up was and is associated with oblique rifting. That includes break-up in the Southern and Equatorial Atlantic, separation from eastern and western Gondwana as well as many recent rift systems, like Gulf of California, Ethiopia Rift and Dead Sea fault. Using a simple analytic mechanical model and advanced numerical, thermomechanical modeling techniques we investigate the influence of oblique extension on the required tectonic force in a three-dimensional setting. While magmatic processes have been already suggested to affect rift evolution, we show that additional mechanisms emerge due to the three-dimensionality of an extensional syst…

Atmospheric Sciencegeographygeography.geographical_feature_categoryRiftEcologyBreak-UpDeformation (mechanics)PaleontologySoil ScienceOblique caseForestryAquatic ScienceFault (geology)OceanographyGondwanaTectonicsGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Rift zoneSeismologyGeologyEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research: Solid Earth
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