Search results for "sea level"

showing 10 items of 123 documents

Overirradiance (Cloud Enhancement) Events at High Latitudes

2013

Contrary to intuition, solar irradiance peaks at partially cloudy conditions. Clouds can boost sunlight by over 1.5 times, even at high latitudes. Depending on cloud velocity, the bursts last from seconds to minutes. Measuring irradiance on a tilted surface with 10-ms resolution allows for a detailed study of such events in Southern Norway, almost at sea level. All monthly maxima from April through September 2011 exceeded 1300 W/m2. The slow sensor registered an annual maximum of 1413 W/m2, while the fast sensor's range was found insufficient. A burst reaching 1528 W/m2 was registered in June 2012. Near the Equator, bursts exceeding 1800 W/m2 have been observed. These numbers are striking s…

SunlightForward scatterEquatorPhotovoltaic systemIrradianceEnvironmental scienceElectrical and Electronic EngineeringCondensed Matter PhysicsSolar irradianceAtmospheric sciencesSea levelElectronic Optical and Magnetic MaterialsLatitudeIEEE Journal of Photovoltaics
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Europe's offshore winds assessed with synthetic aperture radar, ASCAT and WRF

2020

Europe's offshore wind resource mapping is part of the New European Wind Atlas (NEWA) international consortium effort. This study presents the results of analysis of synthetic aperture radar (SAR) ocean wind maps based on Envisat and Sentinel-1 with a brief description of the wind retrieval process and Advanced Scatterometer (ASCAT) ocean wind maps. The wind statistics at 10 and 100 m above mean sea level (a.m.s.l.) height using an extrapolation procedure involving simulated long-term stability over oceans are presented for both SAR and ASCAT. Furthermore, the Weather Research and Forecasting (WRF) offshore wind atlas of NEWA is presented. This has 3 km grid spacing with data …

Synthetic aperture radar010504 meteorology & atmospheric sciencesMeteorologyRenewable Energy Sustainability and the Environmentlcsh:TJ807-8300211 other engineering and technologieslcsh:Renewable energy sourcesEnergy Engineering and Power Technology02 engineering and technologyScatterometer01 natural sciencesWind speedOffshore wind powerWeather Research and Forecasting ModelWind atlasSubmarine pipelineGeologySea level021101 geological & geomatics engineering0105 earth and related environmental sciencesWind Energy Science
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Description of two new fossil echinoids (Echinodermata: Echinoidea) from the Early Hauterivian (Early Cretaceous) of the Paris Basin (France)

2012

International audience; Deux nouveaux genres et espèces d'échinides, Salvaster roberti gen. et sp. nov. et Pygolampas edita gen. et sp. nov. provenant de la Formation des Calcaires à Spatangues (CSF) sont décrits. La CSF correspond à des sédiments calcaréo-argileux déposés dans le sud-est du bassin de Paris (France) à l'Hauterivien inférieur (Crétacé inférieur). Ces dépôts sont datés de la chronozone à Acanthodiscus radiatus, un intervalle de temps qui a correspondu à un haut niveau marin général en Europe de l'Ouest. La CSF a pourtant livré une riche faune fossile d'environnement marin peu profond, principalement représentée par des invertébrés benthiques. Parmi ceux-ci, 54 espèces d'échin…

Systematics010506 paleontologynouveau genrenouvelle espèceFaunaCassiduloida[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural sciencesPaleontologysystématiqueAnimaliaEcology Evolution Behavior and SystematicsSea level0105 earth and related environmental sciencesInvertebrateHauterivienTaxonomyHolasteroidabiologyEcology[ SDU.STU ] Sciences of the Universe [physics]/Earth SciencesEchinoideaBiodiversitybiology.organism_classificationCretaceousNotAcanthodiscus[SDU.STU] Sciences of the Universe [physics]/Earth SciencesAnimal Science and ZoologyChronozoneCassiduloidaEchinodermata
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Middle to Upper Pleistocene morphostructural evolution of the NW-coast of Sicily: thermoluminescence dating and palaeontological-stratigraphical eval…

1997

Abstract Infralittoral and terrigenous Middle to Upper Pleistocene deposits outcropping at the NW-coast of Sicily (Gulf of Castellammare and peninsula of Capo San Vito) were investigated in order to recognise glacio-eustatically caused sea level highstands and the interference between tectonics, eustasy and local conditions of the coast. The results, originating from a stratigraphically important area, were obtained by palaeontological-stratigraphical analyses, physical age determination with the thermoluminescence method and by detailed morphostructural studies. The marine deposits, situated at 3–40 m a.s.l., mainly provide an oligotypic molluscan fauna referable to modern SGCF-, SFHN- and…

Thermoluminescence datingPleistoceneOutcropTerrigenous sedimentPaleontologyOceanographyDeep seaPaleontologyStage (stratigraphy)Glacial periodEcology Evolution Behavior and SystematicsGeologySea levelEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Deep stratosphere-to-troposphere transport (STT) over SE Europe: a complex case study captured by enhanced <sup>7</sup>Be…

2005

Abstract. In this study we present a complex case study of a Stratosphere-to-Troposphere Transport (STT) event down to the surface of a low topography region in Northern Greece, during the second fortnight of March 2000. During this event our surface station at Livadi (23°15 E/40°32 N, 850 m a.s.l.), was influenced by very different synoptic systems developing over Eastern Europe, N. America and the N. Atlantic, the last one evolving to a cut-off low over France/Spain. This is the first study, to our knowledge, that presents a down to the surface STT event in the eastern Mediterranean. The intrusion is primarily captured with the use of the cosmogenic radionuclide 7Be, which increased to 9.…

TroposphereIntrusionRadionuclideEastern mediterraneanPotential vorticityClimatologyConjunction (astronomy)Environmental scienceStratosphereSea level
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Benthic foraminifera as indicators of relative sea-level fluctuations: Paleoenvironmental and paleoclimatic reconstruction of a Holocene marine succe…

2017

This study presents the results of an integrated stratigraphic analysis conducted on a marine gravity core (MSK-12 C4) recovered from the outer continental shelf (82 mwater depth) of western Calabria, ~2.6 km, NE of Capo Vaticano (Eastern Tyrrhenian margin). The gravity core MSK-12 C4 recovered a stratigraphic succession of 4.18 m beneath the seafloor representing the last ~11.1 ka. Sedimentological analysis, micropaleontological quantitative analysis on benthic foraminiferal assemblages, tephrostratigraphy, sequence stratigraphic analysis of high resolution reflection seismic data recorded in the core site area and AMS 14C absolute age determinations allowed reconstructing the marine recor…

Tyrrhenian Sea010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaHolocene climatic optimum010502 geochemistry & geophysics01 natural sciencesForaminiferaPaleontologyAbsolute datingSea levelHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesStable isotopesgeographyIntegrated stratigraphygeography.geographical_feature_categoryPaleoenvironmental and paleoclimatic reconstructionbiologyContinental shelfBenthic foraminiferaSettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationStable isotopeSeafloor spreadingSettore GEO/08 - Geochimica E VulcanologiaOceanographyBenthic zoneLittle Ice AgeGeology
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Sea-level changes during the last 41,000 years in the outer shelf of the southern Tyrrhenian Sea: Evidence from benthic foraminifera and seismostrati…

2011

Abstract An integrated high resolution study based both on a seismostratigraphic approach and on a sedimentary core (VIB 10), collected in the outer shelf (127 m depth) from the southern Tyrrhenian Sea (Gulf of Termini, Sicily), provides new data about climatic, eustatic and paleoenvironmental changes during the last ∼41,000 years. The results based on the interpretation of a seismic profile, on benthic foraminifera assemblages and on δ18O records, allowed recognition of two drastic sea-level falls during the Last Glacial Maximum (LGM) and the Younger Dryas (YD). The short deglacial event, between LGM and YD, known as Bolling/Allerod, played an important role in the sea-level rise that prod…

Tyrrhenian Sea010506 paleontologySettore GEO/02 - Geologia Stratigrafica E Sedimentologicaδ18O[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Holocene climatic optimumbenthic foraminifera[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]010502 geochemistry & geophysics01 natural sciencesAllerød oscillationstable isotopes.ForaminiferaSea-level changeSea-level changes; Tyrrhenian Sea; benthic foraminifera; seismostratigraphic analysis; stable isotopes.14. Life underwaterYounger DryasSea levelComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyLast Glacial MaximumSettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationOceanography13. Climate actionBenthic zoneseismostratigraphic analysiGeology
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Water transfer from Basilicata to Puglia: a technical, economic and institutional challenge

2007

The necessity of supplying Puglia by transfer of water resources from Basilicata (250 Mm/year mainly for civil use but also for agricultural and industrial uses) and another bordering region (Campania for 200 Mm/year only for civil use) arises from the scarcity of water resources inside Puglia, where precipitation is very low (400 mm/year), rivers are few and with limited watersheds and costal aquifers are overexploited with salt intrusion. Moreover recent droughts have pointed out the need for revising water supply policy in Puglia, looking for the increment of the transfer of water resources from Basilicata (50 Mm/year) and Campania (32 Mm/year) and the development of feasibility studies …

Water resourcesWater transferEnvironmental protectionbusiness.industryAgriculturekarst cave sea levelEnvironmental scienceWater supplyWater industrybusinessEnvironmental planningWater Resources Management IV
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Air-sea interaction in the Central Mediterranean: are surge-generating winds changing ?

2009

International audience; Hourly sea surges from the records of 9 French and 19 Italian tide-gauge stations have been computed and the wind directions corresponding to significant surge heights have been determined. The frequency of such surge-related wind directions tends to increase almost everywhere, while extreme wind speeds (that are most effective to produce high surges) tend generally to decrease; this may be a consequence of the northward displacement of storm trajectories on the European area. There is, however, an exception in the Gulf of Lions (the most westward area considered), where surge height may reach higher elevations, with a recent dangerous increase of southerlies

[ SDU.OCEAN ] Sciences of the Universe [physics]/Ocean Atmosphere[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere[SDU.OCEAN] Sciences of the Universe [physics]/Ocean Atmosphere[SDE.MCG]Environmental Sciences/Global Changestide gaugesea levelMediterranean[ SDE.MCG ] Environmental Sciences/Global Changes[SDE.MCG] Environmental Sciences/Global Changes[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatologyclimate change[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatologywind[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatologysurge
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Sedimentation and tropical vegetation changes in Southern Benin (West Africa), carbon-13 tracing of organic matter dynamics and fluctuations of the s…

2007

International audience

[SDE] Environmental Sciencesmangrovepaleoenvironmentfacies deltaiques[SDV]Life Sciences [q-bio]rapport isotopique 13C/12Cfluctuation du niveau marinpaleoenvironnement[SDV] Life Sciences [q-bio]13c/12c isotope ratioOuémé-Sô[SDE]Environmental Sciencessea level fluctuationdelta faciesComputingMilieux_MISCELLANEOUS
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