Search results for "water"

showing 10 items of 9348 documents

Mercury emissions from soils and fumaroles of Nea Kameni volcanic centre, Santorini (Greece)

2013

There have been limited studies to date targeting mercury emissions from volcanic fumarolic systems, and no mercury flux data exist for soil or fumarolic emissions at Santorini volcanic complex, Greece. We present results from the first geochemical survey of Hg and major volatile (CO2, H2S, H2O and H-2) concentrations and fluxes in the fumarolic gases released by the volcanic/hydrothermal system of Nea Kameni islet; the active volcanic center of Santorini. These data were obtained using a portable mercury spectrometer (Lumex 915+) for gaseous elemental mercury (GEM) determination, and a Multi-component Gas Analyzer System (Multi-GAS) for major volatiles. Gaseous Elemental Mercury (GEM) conc…

010504 meteorology & atmospheric sciencesvolcanogenic mercury volcanic degassing Santorini mercury flux inventory trace metalsEarth sciencetrace metalsAir pollutionchemistry.chemical_element010502 geochemistry & geophysicsmedicine.disease_cause01 natural scienceschemistry.chemical_compoundGeochemistry and Petrologymercury flux inventorymedicinevolcanogenic mercuryAir quality index0105 earth and related environmental sciencesgeographySantorinigeography.geographical_feature_categoryFumaroleSettore GEO/08 - Geochimica E VulcanologiaMercury (element)GeophysicschemistryVolcano13. Climate actionEnvironmental chemistryCarbon dioxideSoil watervolcanic degassingGeologyGEOCHEMICAL JOURNAL
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Identification of processes that control the stable isotope composition of rainwater in the humid tropical West-Central Africa.

2020

12 pages; International audience; This study interprets 11 years (2006 to 2016) and 6 months (March to August in 2017) of respectively monthly and daily isotopic (δD and δ18O) monitoring of rain at Douala (Cameroon), a humid tropical station in Western Africa. The main scope is to analyze the climate controls on precipitation isotopes at different timescales. Firstly, we examine the annual cycles of δ18O. Over the 11 years of survey, the annual cycle exhibits a W shape that is quite reproducible from year to year, with two minima in spring and autumn periods. Based on back trajectory calculations and remote sensing observations of water vapor isotopic composition, we show that the observed …

010504 meteorology & atmospheric sciencesδ18O0207 environmental engineeringHumid subtropical climate02 engineering and technologyAtmospheric sciencesAir back trajectory01 natural sciencesGPCP precipitation[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySpring (hydrology)Precipitation020701 environmental engineeringδ18OComputingMilieux_MISCELLANEOUSAir mass0105 earth and related environmental sciencesWater Science and TechnologyWater vapor[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_categoryStable isotope ratioAnnual cycleConvective activity[SDU]Sciences of the Universe [physics]13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyEnvironmental scienceWater vapor
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Insolation cycles as a major control equatorial Indian Ocean primary production

1997

Analysis of a continuous sedimentary record taken in the Maldives indicates that strong primary production fluctuations (70 to 390 grams of carbon per square meter per year) have occurred in the equatorial Indian Ocean during the past 910,000 years. The record of primary production is coherent and in phase with the February equatorial insolation, whereas it shows diverse phase behavior with δ 18 O, depending on the orbital frequency (eccentricity, obliquity, or precession) examined. These observations imply a direct control of productivity in the equatorial oceanic system by insolation. In the equatorial Indian Ocean, productivity is driven by the wind intensity of westerlies, which is rel…

010504 meteorology & atmospheric sciencesδ18Omedia_common.quotation_subject[SDU.STU]Sciences of the Universe [physics]/Earth SciencesForcing (mathematics)010502 geochemistry & geophysics01 natural sciencesPhysics::Geophysics100000-year problem14. Life underwaterEccentricity (behavior)Physics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesmedia_common[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereMultidisciplinaryEquatorial wavesWesterliesOceanographyProductivity (ecology)13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyPhysics::Space PhysicsPrecessionAstrophysics::Earth and Planetary Astrophysics[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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A Geometry-Based Underwater Acoustic Channel Model Allowing for Sloped Ocean Bottom Conditions

2017

This paper proposes a new geometry-based channel model for shallow-water ocean environments, in which the ocean bottom can slope gently down/up. The need for developing such an underwater acoustic (UWA) channel model is driven by the fact that the standard assumption of a flat ocean bottom does not hold in many realistic scenarios. Starting from a geometrical model, we develop a stochastic channel model for wideband single-input single-output vehicle-to-vehicle UWA channels using the ray theory assuming smooth ocean surface and bottom. We investigate the effect of the ocean-bottom slope angle on the distribution of the channel envelope, instantaneous channel capacity, temporal autocorrelati…

010505 oceanographyApplied MathematicsAutocorrelation020206 networking & telecommunicationsGeometry02 engineering and technology01 natural sciencesComputer Science ApplicationsDelay spreadChannel capacity0202 electrical engineering electronic engineering information engineeringElectrical and Electronic EngineeringWidebandUnderwaterPower delay profileGeologyCoherence bandwidthComputer Science::Information Theory0105 earth and related environmental sciencesCommunication channelIEEE Transactions on Wireless Communications
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A Nonisovelocity Geometry-Based Underwater Acoustic Channel Model

2018

This paper proposes a new geometry-based shallow underwater acoustic (UWA) channel model allowing for nonisovelocity ocean conditions. The fact that the isovelocity assumption does not hold in many real-world scenarios motivates the need for developing channel models for nonisovelocity UWA propagation environments. Starting from a geometrical model, we develop a stochastic channel model for a single-input single-output (SISO) vehicle-to-vehicle UWA channel assuming that the ocean surface and bottom are rough and that the speed of sound varies with depth. The effect of the nonisovelocity condition has been assessed regarding its influence on the temporal autocorrelation function, the frequen…

010505 oceanographyComputer Networks and CommunicationsComputer scienceAutocorrelationAerospace Engineering020206 networking & telecommunicationsGeometry02 engineering and technology01 natural sciencesDelay spreadAutomotive Engineering0202 electrical engineering electronic engineering information engineeringElectrical and Electronic EngineeringUnderwaterUnderwater acousticsPower delay profileUnderwater acoustic communicationCoherence bandwidth0105 earth and related environmental sciencesCommunication channelIEEE Transactions on Vehicular Technology
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Performance analysis of Alamouti-coded OFDM systems over spatio-temporally correlated underwater acoustic channels

2017

In this paper, we analyze the performance of Alamouti-coded orthogonal frequency division multiplexing (OFDM) systems over time-varying underwater acoustic (UWA) channels. A realistic UWA channel model has been considered, which can be correlated in either time or space or simultaneously in both domains. An exact analytical expression for the bit error probability (BEP) is necessary to analyze accurately the performance of Alamouti-coded OFDM systems over the spatio-temporally correlated UWA channel model. Hence, by using this UWA channel model, an expression has been derived for the BEP of Alamouti-coded OFDM systems assuming that the receiver knows perfectly the channel state information.…

010505 oceanographyComputer scienceOrthogonal frequency-division multiplexingbusiness.industry05 social sciences050801 communication & media studies01 natural sciencesExpression (mathematics)Computer Science::Performancesymbols.namesake0508 media and communicationsChannel state informationsymbolsWirelessAntenna (radio)UnderwaterbusinessTelecommunicationsDoppler effectAlgorithmComputer Science::Information Theory0105 earth and related environmental sciencesCommunication channel2017 IEEE International Conference on Communications (ICC)
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A sea surface temperature reconstruction for the southern Indian Ocean trade wind belt from corals in Rodrigues Island (19°S, 63°E)

2016

Abstract. The western Indian Ocean has been warming rapidly over recent decades, causing a greater number of extreme climatic events. It is therefore of paramount importance to improve our understanding of links between Indian Ocean sea surface temperature (SST) variability, climate change and sustainability of tropical coral reef ecosystems. Here we present monthly resolved coral Sr ∕ Ca records from two different locations from Rodrigues Island (63° E, 19° S) in the south-central Indian Ocean trade wind belt. We reconstruct SST based on a linear relationship with the Sr ∕ Ca proxy with records starting from 1781 and 1945, respectively. We assess relationships between the observed long-ter…

010506 paleontology010504 meteorology & atmospheric sciences550Corallcsh:LifeClimate changeMonsoon010502 geochemistry & geophysics01 natural sciencesddc:570lcsh:QH540-549.514. Life underwaterEcology Evolution Behavior and SystematicsEarth-Surface Processes0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorySubtropical Indian Ocean Dipolelcsh:QE1-996.5Coral reeflcsh:GeologySea surface temperaturelcsh:QH501-531Oceanography13. Climate actionClimatologyIndian Ocean Dipolelcsh:EcologyGeologyTeleconnection
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Productivity modes in the Mediterranean Sea during Dansgaard–Oeschger (20,000–70,000 yr ago) oscillations

2013

The study of planktonic organisms during abrupt climatic variations of the last glacial period (Dansgaard-Oeschger oscillations, D-O) may reveal important insights on climatic, oceanographic and biological interactions. Here we present planktic foraminifera and coccolithophore data collected at the Ocean Drilling Program Site 963 (Sicily Channel), with a mean sampling resolution of respectively 43.5 and 98.9. yr, over the interval between 70,000 and 20,000. yr ago. The paleoenvironmental reconstruction suggests that three different scenarios can be seen across each D-O cycle: 1. oligotrophic surface water and a deep thermocline for the early Interstadials; 2. a Deep Chlorophyll Maximum and …

010506 paleontology010504 meteorology & atmospheric sciencesCoccolithophoreMediterraneanOceanography01 natural sciencesForaminifera/dk/atira/pure/sustainabledevelopmentgoals/life_below_waterWater columnMediterranean seaPaleoproductivity Dansgaard–Oeschger Mediterranean Planktonic Foraminifera CoccolithophoresCoccolithophores14. Life underwaterStadialGlacial periodSDG 14 - Life Below WaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesDeep chlorophyll maximumbiologyPaleontologybiology.organism_classificationOceanography13. Climate actionClimatologyPlanktonic ForaminiferaDansgaard-OeschgerThermoclineGeologyPaleoproductivityPalaeogeography, Palaeoclimatology, Palaeoecology
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Palaeobiogeography of Austral echinoid faunas: a first quantitative approach

2013

Few studies have been devoted to the palaeobiogeography of Antarctic echinoids, all of them analysing and discussing distribution patterns in a qualitative way. The present work aims at exploring the evolution of palaeobiogeographic relationships of Austral echinoid faunas through four time intervals, from the Maastrichtian to the present day, using a quantitative approach: the Bootstrapped Spanning Network procedure. Analyses were successfully performed and improve our knowledge of biogeographic relationships between the different Austral regions. Biogeographic maps were produced that can be easily and intuitively discussed. Our results mostly agree with palaeobiogeographic studies perform…

010506 paleontology010504 meteorology & atmospheric sciencesFaunaGeologyOcean EngineeringPresent day01 natural sciencesCretaceousPaleontologyOceanographyBenthic zoneCenozoicGeology0105 earth and related environmental sciencesWater Science and TechnologyInvertebrateGeological Society, London, Special Publications
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El Niño variability off Peru during the last 20,000 years

2005

Here we present a high-resolution marine sediment record from the El Nino region off the coast of Peru spanning the last 20,000 years. Sea surface temperature, photosynthetic pigments, and a lithic proxy for El Nino flood events on the continent are used as paleo–El Nino–Southern Oscillation proxy data. The onset of stronger El Nino activity in Peru started around 17,000 calibrated years before the present, which is later than modeling experiments show but contemporaneous with the Heinrich event 1. Maximum El Nino activity occurred during the early and late Holocene, especially during the second and third millennium B.P. The recurrence period of very strong El Nino events is 60–80 years. El…

010506 paleontology010504 meteorology & atmospheric sciencesFlood mythNorthern HemispherePaleontologyOceanography01 natural sciencesSea surface temperatureOceanographyEl Niño Southern OscillationEl Niño13. Climate actionClimatology14. Life underwaterYounger DryasHoloceneGeology0105 earth and related environmental sciencesPaleoceanography
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