Search results for "H50"

showing 10 items of 37 documents

Assessing long-term fiscal developments : a new approach

2011

We use a new approach to assess long-term fiscal developments. By analyzing the time-varying behaviour of the two components of government spending and revenue – responsiveness and persistence–, a feature not captured by automatic stabilisers, we are able to infer about the sources of fiscal deterioration (improvement). Drawing on quarterly data, we estimate recursively these components within a system of government revenue and spending equations using a Three-Stage Least Square method for eight European Union countries plus the US. The results suggest that significant changes in the fiscal stance (including those related to the current crisis) are reflected in the estimates of persistence …

MacroeconomicsEconomics and Econometricsjel:E62Fiscal deterioration Fiscal SustainabilitySocial SciencesFinanzpolitikFiscal SustainabilityFiscal deteriorationFiscal DeteriorationÖffentlicher HaushaltPolitischer Konjunkturzyklus0502 economics and businessFiscal Deterioration fiscal sustainabilityddc:330EconomicsRevenuemedia_common.cataloged_instance050207 economicsEuropean unionH50Dezentralisierung050205 econometrics media_commonGovernment spendingFiscalFiscal Deterioration Fiscal Sustainability.05 social sciencesSettore SECS-P/02 Politica Economicajel:H50Fiscal sustainabilityTerm (time)Government revenuePanelEU-StaatenFiscal sustainabilityE62Öffentliche AusgabenFinance
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Gleason parts for algebras of holomorphic functions on the ball of $\mathbf{c_0}$

2019

For a complex Banach space $X$ with open unit ball $B_X,$ consider the Banach algebras $\mathcal H^\infty(B_X)$ of bounded scalar-valued holomorphic functions and the subalgebra $\mathcal A_u(B_X)$ of uniformly continuous functions on $B_X.$ Denoting either algebra by $\mathcal A,$ we study the Gleason parts of the set of scalar-valued homomorphisms $\mathcal M(\mathcal A)$ on $\mathcal A.$ Following remarks on the general situation, we focus on the case $X = c_0.$

Mathematics - Functional AnalysisMathematics::Functional AnalysisFOS: Mathematics46J15 30H50 46E50 30H05Functional Analysis (math.FA)
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Scaling carbon fluxes from eddy covariance sites to globe: synthesis and evaluation of the FLUXCOM approach

2020

FLUXNET comprises globally distributed eddy-covariance-based estimates of carbon fluxes between the biosphere and the atmosphere. Since eddy covariance flux towers have a relatively small footprint and are distributed unevenly across the world, upscaling the observations is necessary to obtain global-scale estimates of biosphere–atmosphere exchange. Based on cross-consistency checks with atmospheric inversions, sun-induced fluorescence (SIF) and dynamic global vegetation models (DGVMs), here we provide a systematic assessment of the latest upscaling efforts for gross primary production (GPP) and net ecosystem exchange (NEE) of the FLUXCOM initiative, where different machine learning methods…

Meteorologie en Luchtkwaliteit010504 meteorology & atmospheric sciencesMeteorology and Air Qualitylcsh:LifeEddy covarianceFlux010501 environmental sciencesAtmospheric sciences01 natural sciencesCarbon cycle03 medical and health sciencesFluxNetLaboratory of Geo-information Science and Remote Sensinglcsh:QH540-549.5ddc:550Life ScienceLaboratorium voor Geo-informatiekunde en Remote SensingBiogeosciences[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentScalingEcology Evolution Behavior and Systematics030304 developmental biology0105 earth and related environmental sciencesCarbon fluxEarth-Surface ProcessesSDG 15 - Life on Land[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere0303 health sciencesWIMEKlcsh:QE1-996.5Carbon sinkBiospherePrimary production15. Life on landlcsh:GeologyEarth scienceslcsh:QH501-53113. Climate actionGreenhouse gasEnvironmental sciencelcsh:Ecology
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Methanotrophic activity and diversity of methanotrophs in volcanic geothermal soils at Pantelleria (Italy)

2014

Volcanic and geothermal systems emit endogenous gases by widespread degassing from soils, including CH4, a greenhouse gas twenty-five times as potent as CO2. Recently, it has been demonstrated that volcanic or geothermal soils are not only a source of methane, but are also sites of methanotrophic activity. Methanotrophs are able to consume 10–40 Tg of CH4 a−1 and to trap more than 50% of the methane degassing through the soils. We report on methane microbial oxidation in the geothermally most active site of Pantelleria (Italy), Favara Grande, whose total methane emission was previously estimated at about 2.5 Mg a−1 (t a−1). Laboratory incubation experiments with three top-soil samples from …

Methane oxidationMethane monooxygenaselcsh:LifeSettore BIO/19 - Microbiologia GeneraleMethanechemistry.chemical_compoundlcsh:QH540-549.5Soil pHEcology Evolution Behavior and SystematicsEarth-Surface ProcessesbiologyEcologylcsh:QE1-996.5bacterial diversityAlphaproteobacteriaVerrucomicrobiabiology.organism_classificationMethanotrophSettore GEO/08 - Geochimica E Vulcanologialcsh:Geologylcsh:QH501-531chemistryEnvironmental chemistryMethane emissionAnaerobic oxidation of methaneSoil waterbiology.proteinSoil horizonlcsh:EcologyBiogeosciences
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Nitrous oxide emission budgets and land-use-driven hotspots for organic soils in Europe

2014

Organic soils are a main source of direct emissions of nitrous oxide (N2O), an important greenhouse gas (GHG). Observed N2O emissions from organic soils are highly variable in space and time, which causes high uncertainties in national emission inventories. Those uncertainties could be reduced when relating the upscaling process to a priori-identified key drivers by using available N2O observations from plot scale in empirical approaches. We used the empirical fuzzy modelling approach MODE to identify main drivers for N2O and utilize them to predict the spatial emission pattern of European organic soils. We conducted a meta-study with a total amount of 659 annual N2O measurements, which was…

N-DEPOSITION1171 GeosciencesPeat010504 meteorology & atmospheric sciencesGRASSLANDWater tableeducationlcsh:LifeGreenhouse gas inventorySoil scienceAtmospheric sciences01 natural sciencesGrasslandSoil pHlcsh:QH540-549.5media_common.cataloged_instanceAGRICULTURAL SOILSEuropean unionEcology Evolution Behavior and Systematics1172 Environmental sciences0105 earth and related environmental sciencesEarth-Surface Processesmedia_commongeographyPOLICY SUPPORT4112 Forestrygeography.geographical_feature_categoryCH4lcsh:QE1-996.504 agricultural and veterinary sciences15. Life on landWATER-TABLEPEAT SOILSlcsh:Geologylcsh:QH501-53113. Climate actionGreenhouse gasSoil waterNORTHERN PEATLANDS040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceCO2lcsh:EcologyN2O FLUXES
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Bioaerosols in the Amazon rain forest: temporal variations and vertical profiles of Eukarya, Bacteria, and Archaea

2021

The Amazon rain forest plays a major role in global hydrological cycling, and biogenic aerosols are likely to influence the formation of clouds and precipitation. Information about the sources and altitude profiles of primary biological aerosol particles, however, is sparse. We used fluorescence in situ hybridization (FISH), a molecular biological staining technique largely unexplored in aerosol research, to investigate the sources and spatiotemporal distribution of Amazonian bioaerosols on the domain level. We found wet season bioaerosol number concentrations in the range of 1–5 × 105 m−3 accounting for > 70 % of the coarse mode aerosol. Eukaryotic and bacterial particles predominated, …

QE1-996.5EcologyAmazonianIndoor bioaerosolGeologyUnderstoryAtmospheric sciencesAerosolAltitudeBioprecipitationLifeQH501-531Environmental sciencePrecipitationEcology Evolution Behavior and SystematicsQH540-549.5Earth-Surface ProcessesBioaerosol
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Bifurcations in the elementary Desboves family

2017

International audience; We give an example of a family of endomorphisms of $\mathbb{P}^2(\mathbb{C})$ whose Julia set depends continuously on the parameter and whose bifurcation locus has non-empty interior.

[ MATH ] Mathematics [math]Pure mathematicsEndomorphismMathematics - Complex VariablesApplied MathematicsGeneral Mathematics010102 general mathematicsDynamical Systems (math.DS)MSC: 32H50 37F4516. Peace & justice01 natural sciencesJulia setDynamicsRational mapsBifurcation locus0103 physical sciencesFOS: Mathematics32H50 37F45 37F50010307 mathematical physics0101 mathematics[MATH]Mathematics [math]Complex Variables (math.CV)Mathematics - Dynamical SystemsMathematics
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Modelling biogeochemical processes in sediments from the north-western Adriatic Sea: response to enhanced particulate organic carbon fluxes

2018

This work presents the result of a study carried out in the north-western Adriatic Sea, by combining two different types of biogeochemical models with field sampling efforts. A longline mussel farm was taken as a local source of perturbation to the natural particulate organic carbon (POC) downward flux. This flux was first quantified by means of a pelagic model of POC deposition coupled to sediment trap data, and its effects on sediment bioirrigation capacity and organic matter (OM) degradation pathways were investigated constraining an early diagenesis model by using original data collected in sediment porewater. The measurements were performed at stations located inside and outside the ar…

[ SDU.OCEAN ] Sciences of the Universe [physics]/Ocean Atmosphere0106 biological sciencesSettore BIO/07 - EcologiaBiogeochemical cycle010504 meteorology & atmospheric sciencesMARINE-SEDIMENTSEARLY-DIAGENESISlcsh:LifeMEDITERRANEAN LAGOONMUSSEL CULTURE01 natural sciencesNITROGEN DYNAMICS[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistrylcsh:QH540-549.5Dissolved organic carbon[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentbiogeochemistry marine sediments carbon fluxesOrganic matter14. Life underwaterDYNAMIC ENERGY BUDGETComputingMilieux_MISCELLANEOUSEcology Evolution Behavior and Systematics[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography0105 earth and related environmental sciencesEarth-Surface Processeschemistry.chemical_classificationTotal organic carbonSULFATE REDUCTION010604 marine biology & hydrobiologylcsh:QE1-996.5BioirrigationBiogeochemistrySedimentWATER INTERFACEMusselDYNAMIC ENERGY BUDGET EARLY-DIAGENESIS WATER INTERFACE MUSSEL CULTURE MEDITERRANEAN LAGOON NITROGEN DYNAMICS COASTAL SEDIMENTS SULFATE REDUCTION NUTRIENT DYNAMICS MARINE-SEDIMENTSNUTRIENT DYNAMICSlcsh:Geologylcsh:QH501-531Oceanographychemistry13. Climate actionEnvironmental sciencelcsh:EcologyCOASTAL SEDIMENTSDYNAMIC ENERGY BUDGET; EARLY-DIAGENESIS; WATER INTERFACE; MUSSEL CULTURE; MEDITERRANEAN LAGOON; NITROGEN DYNAMICS; COASTAL SEDIMENTS; SULFATE REDUCTION; NUTRIENT DYNAMICS; MARINE-SEDIMENTS
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Assessing the potential long-term increase of oceanic fossil fuel CO2 uptake due to CO2-calcification feedback

2007

International audience; Plankton manipulation experiments exhibit a wide range of sensitivities of biogenic calcification to simulated anthropogenic acidification of the ocean, with the "lab rat" of planktic calcifiers, Emiliania huxleyi apparently not representative of calcification generally. We assess the implications of this observational uncertainty by creating an ensemble of realizations of an Earth system model that encapsulates a comparable range of uncertainty in calcification response to ocean acidification. We predict that a substantial reduction in marine carbonate production is possible in the future, with enhanced ocean CO2 sequestration across the model ensemble driving a 4?1…

[ SDU.OCEAN ] Sciences of the Universe [physics]/Ocean Atmosphere[SDU.OCEAN] Sciences of the Universe [physics]/Ocean Atmospherelcsh:QE1-996.5fungilcsh:Life[ SDU.STU ] Sciences of the Universe [physics]/Earth Sciences[SDU.ASTR] Sciences of the Universe [physics]/Astrophysics [astro-ph][ PHYS.ASTR.CO ] Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO][SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentlcsh:Geologylcsh:QH501-531[PHYS.ASTR.CO] Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]lcsh:QH540-549.5[SDU.STU] Sciences of the Universe [physics]/Earth Sciences[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentlcsh:Ecology[ SDU.ASTR ] Sciences of the Universe [physics]/Astrophysics [astro-ph]
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The unique skeleton of siliceous sponges (Porifera; Hexactinellida and Demospongiae) that evolved first from the Urmetazoa during the Proterozoic: a …

2007

Abstract. Sponges (phylum Porifera) had been considered as an enigmatic phylum, prior to the analysis of their genetic repertoire/tool kit. Already with the isolation of the first adhesion molecule, galectin, it became clear that the sequences of the sponge cell surface receptors and those of the molecules forming the intracellular signal transduction pathways, triggered by them, share high similarity to those identified in other metazoan phyla. These studies demonstrated that all metazoan phyla, including the Porifera, originate from one common ancestor, the Urmetazoa. The sponges evolved during a time prior to the Ediacaran-Cambrian boundary (542 million years ago (myr)). They appeared du…

biologyPhylum[SDU.OCEAN] Sciences of the Universe [physics]/Ocean Atmospherelcsh:QE1-996.5lcsh:Lifemyrbiology.organism_classification[SDU.ASTR] Sciences of the Universe [physics]/Astrophysics [astro-ph][SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentSuberites domunculaIntracellular signal transductionlcsh:GeologySpongelcsh:QH501-531Body planSponge spiculeEvolutionary biology[PHYS.ASTR.CO] Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]lcsh:QH540-549.5Botany[SDU.STU] Sciences of the Universe [physics]/Earth Scienceslcsh:EcologyLiving fossilEcology Evolution Behavior and SystematicsEarth-Surface Processes
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