Search results for "Wind-Speed"

showing 2 items of 2 documents

Persistence in complex systems

2022

Persistence is an important characteristic of many complex systems in nature, related to how long the system remains at a certain state before changing to a different one. The study of complex systems' persistence involves different definitions and uses different techniques, depending on whether short-term or long-term persistence is considered. In this paper we discuss the most important definitions, concepts, methods, literature and latest results on persistence in complex systems. Firstly, the most used definitions of persistence in short-term and long-term cases are presented. The most relevant methods to characterize persistence are then discussed in both cases. A complete literature r…

fractal dimensionFOS: Computer and information sciencesComplex systemsRenewable energyglobal solar-radiationsystems' statesComplex networksGeneral Physics and AstronomyFOS: Physical scienceslong-term and short-term methodsadaptationzero-temperature dynamicsDynamical Systems (math.DS)Physics - GeophysicsneurosciencememoryMethodology (stat.ME)PersistenceOptimization and planningMemoryMachine learningearthquake magnitude seriesFOS: MathematicsAtmosphere and climateMathematics - Dynamical SystemsAdaptationcomplex systemslow-visibility eventstime-seriesStatistics - Methodologyinflation persistenceLong-term and short-term methodsdetrended fluctuation analysislong-range correlationspersistencecomplex networksSystems’ statesEconomyneural networksrenewable energyGeophysics (physics.geo-ph)atmosphere and climateeconomymachine learningoptimization and planningNeural networkswind-speedNeuroscience
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Global sea-to-air flux climatology for bromoform, dibromomethane and methyl iodide

2013

Volatile halogenated organic compounds containing bromine and iodine, which are naturally produced in the ocean, are involved in ozone depletion in both the troposphere and stratosphere. Three prominent compounds transporting large amounts of marine halogens into the atmosphere are bromoform (CHBr3), dibromomethane (CH2Br2) and methyl iodide (CH3I). The input of marine halogens to the stratosphere has been estimated from observations and modelling studies using low-resolution oceanic emission scenarios derived from top-down approaches. In order to improve emission inventory estimates, we calculate data-based high resolution global sea-to-air flux estimates of these compounds from surface ob…

[SDE] Environmental SciencesAtmospheric Science010504 meteorology & atmospheric sciences[SDV]Life Sciences [q-bio]Tropical Tropopause LayerWind-Speed010501 environmental sciencesAtmospheric sciences01 natural sciencesDibromomethaneTroposphereAtmospherelcsh:ChemistryStratospheric Brominechemistry.chemical_compoundFlux (metallurgy)Ocean gyrePhysical Sciences and MathematicsGas-ExchangeOzone Depletion14. Life underwaterEmission inventoryStratosphere0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryAtlantic-OceanLife SciencesOzone depletionlcsh:QC1-999Halogenated Organic-Compounds[SDV] Life Sciences [q-bio]chemistrylcsh:QD1-99913. Climate actionMarine Boundary-LayerClimatologyPhytoplankton Cultures[SDE]Environmental SciencesPhotochemical Productionlcsh:Physics
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