Search results for "Radiative forcing"

showing 10 items of 60 documents

Temperature Covariance in Tree Ring Reconstructions and Model Simulations Over the Past Millennium

2017

Spatial covariance in the simulated temperature evolution over the past millennium has been reported to exceed that of multiproxy-based reconstructions. Here we use tree ring-based temperature reco ...

010504 meteorology & atmospheric sciencesCovariance functionDendroclimatologyRadiative forcingCovariance010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesGeophysicsClimatologyPaleoclimatologyDendrochronologyGeneral Earth and Planetary SciencesSpatial variabilityGeology0105 earth and related environmental sciencesGeophysical Research Letters
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Effect of the Ordovician paleogeography on the (in)stability of the climate.

2014

The Ordovician Period (485–443 Ma) is characterized by abundant evidence for continental-sized ice sheets. Modeling studies published so far require a sharp CO2 drawdown to initiate this glaciation. They mostly used non-dynamic slab mixed-layer ocean models. Here, we use a general circulation model with coupled components for ocean, atmosphere, and sea ice to examine the response of Ordovician climate to changes in CO2 and paleogeography. We conduct experiments for a wide range of CO2 (from 16 to 2 times the preindustrial atmospheric CO2 level (PAL)) and for two continental configurations (at 470 and at 450 Ma) mimicking the Middle and the Late Ordovician conditions. We find that the temper…

010504 meteorology & atmospheric scienceslcsh:Environmental protectionStratigraphy010502 geochemistry & geophysics01 natural scienceslcsh:Environmental pollutionSea icelcsh:TD169-171.8Glacial periodlcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350Global and Planetary Changegeographygeography.geographical_feature_categoryNorthern HemispherePaleontologyRadiative forcingOcean dynamics13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU]Sciences of the Universe [physics]Climatologylcsh:TD172-193.5OrdovicianIce sheet[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyGlobal coolingGeology[ SDU ] Sciences of the Universe [physics]
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Winter climate signal in boreal clastic-biogenic varves : a comprehensive analysis of three varved records from 1890 to 1990 AD with meteorological a…

2017

Clastic-biogenic varves are widely used for reconstructing past climate: in boreal environments, the accumulation of minerogenic clasts on the lake floor is generally considered a proxy for past variations in spring floods reflecting previous winter conditions. However, the physical mechanisms behind this winter climate sensitivity and the influence of catchment type on the varve formation are not fully investigated. Here, we present a winter climate record inferred from the clastic laminae of three lakes located on the region of fine-grained tills in Eastern Finland spanning from AD 1890 to 1990. The minerogenic varve data are compared with instrumental meteorological and hydrological time…

010506 paleontology010504 meteorology & atmospheric sciencesta1172ta1171Drainage basinlake sedimentsNorthern Europecatchment dynamics01 natural sciencesProxy (climate)clastic-biogenic varvesta2180105 earth and related environmental sciencesgeographyVarvegeography.geographical_feature_categoryPaleontologyGeology15. Life on landRadiative forcingSubarctic climateclimate forcingBoreal13. Climate actionClastic rockClimatologyfine-grained tillsClimate sensitivityGeologyboreal climateGFF
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Volcanic climate forcing preceding the inception of the Younger Dryas: Implications for tracing the Laacher See eruption

2021

Climatic warming from the last glacial maximum to the current interglacial period was punctuated by a similar to 1300 years long cold period, commonly referred to as the Younger Dryas (YD). Several hypotheses have been proposed for the mechanism triggering the abrupt inception of the YD, including freshwater forcing, an extra-terrestrial impact, and aerosols from volcanic eruptions. Here, we use synchronised sulphate and sulphur records from both Greenland and Antarctic ice cores to reconstruct volcanic forcing between 13,200-12,800 a BPGICC05 (years before 1950 CE on the Greenland Ice Core Chronology 2005; GICC05). This continuous reconstruction of stratospheric sulphur injections highligh…

010506 paleontologyArcheologyYounger Dryas010504 meteorology & atmospheric sciences530 PhysicsCIRCULATIONIce cores; Laacher See eruption; Sulphate; Volcanic radiative forcing; Younger DryasSULFURForcing (mathematics)01 natural sciencesVolcanic radiative forcingANTARCTIC ICE-CORESOCEANIce coreCHRONOLOGYYounger Dryas550 Earth sciences & geologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary Changegeographygeography.geographical_feature_categoryGeologyLast Glacial MaximumRECORDWAIS DIVIDESulphateRadiative forcingGREENLANDLaacher See eruptionVolcano13. Climate actionIce coresClimatologySYNCHRONIZATIONInterglacialClimate modelSULFATEGeologyQuaternary Science Reviews
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Regional and Supra-Regional Coherence in Limnological Variabler

2009

Limnologists and water resources managers have traditionally perceived lakes as discrete geographical entities. This has resulted in a tendency for scientific lake studies to concentrate on lakes as individuals, with little connection either to each other or to large-scale driving forces. Since the 1990s, however, a shift in the prevailing paradigm has occurred, with lakes increasingly being seen as responding to regional, rather than local, driving forces. The seminal work on regional coherence in lake behaviour was that of Magnuson et al. (1990), who showed that many features of lakes within the same region respond coherently to drivers such as climate forcing and catchment processes. Fro…

0106 biological sciencesgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesCatchment ModellingEcology010604 marine biology & hydrobiologyClimate ChangeDrainage basinClimate changeCoherence (statistics)Lake ModellingRadiative forcing01 natural sciencesWater resourcesSpatial coherence13. Climate actionNorth Atlantic oscillationBiological propertyddc:570Water QualityPhysical geography0105 earth and related environmental sciences
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Microbiology and atmospheric processes: research challenges concerning the impact of airborne micro-organisms on the atmosphere and climate

2011

 Cet article a fait l'objet d'une discussion dans "Morris, C. E., Sands, D. C., Bardin, M., Jaenicke, R., Vogel, B., Leyronas, C., Ariya, P. A., and Psenner, R.: Microbiology and atmospheric processes: an upcoming era of research on bio-meteorology, Biogeosciences Discuss., 5, 191-212, doi:10.5194/bgd-5-191-2008, 2008."; International audience; For the past 200 years, the field of aerobiology has explored the abundance, diversity, survival and transport of micro-organisms in the atmosphere. Micro-organisms have been explored as passive and severely stressed riders of atmospheric transport systems. Recently, an interest in the active roles of these micro-organisms has emerged along with prop…

AIRBORNE DISSEMINATION010504 meteorology & atmospheric sciencesMeteorologyAEROBIOLOGY;BIOLOGICAL AEROSOLS;BIO-METEOROLOGY;TRANSPORT;AIRBORNE DISSEMINATION;BIOLOGICAL PROPERTIES;ATMOSPHERIC PROCESSES;BIOSPHERE;CLIMATE CHANGEEarth scienceBiomeCLIMATE CHANGEBiological particleslcsh:Lifemodélisation spatialeBIOSPHERE010501 environmental sciencesBiologyAtmosphere (architecture and spatial design)01 natural sciencesBIO-METEOROLOGYATMOSPHERIC PROCESSESBIOLOGICAL AEROSOLSlcsh:QH540-549.5AEROBIOLOGYddc:550microbiologieEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processeschangement climatiquemicroorganismeBIOLOGICAL PROPERTIESclimatlcsh:QE1-996.5microorganisme aerienRadiative forcingTRANSPORT[SDV.BBM.BC]Life Sciences [q-bio]/Biochemistry Molecular Biology/Biomolecules [q-bio.BM]lcsh:GeologyEarth sciencesatmosphèrelcsh:QH501-53113. Climate actionAtmospheric chemistrylcsh:EcologyMetabolic activityBiogeosciences
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A Comparative Analysis of Aerosol Microphysical, Optical and Radiative Properties during the Spring Festival Holiday over Beijing and Surrounding Reg…

2018

ABSTRACT Using ground-based data, meteorological observations, and atmospheric environmental monitoring data, a comparative analysis of the microphysical and optical properties, and radiative forcing of aerosols was conducted between three stations in different developed environments during a severe air pollution episode during the Spring Festival over Beijing. During the most polluted period, the daily peak values of the aerosol optical depth were ~1.62, ~1.73, and ~0.74, which were about 2.6, 2.9, and 2.1 times higher than the background levels at the CAMS, Xianghe, and Shangdianzi sites, respectively. The daily peak values of the single scattering albedo were ~0.95, ~0.96, and ~0.87. The…

AerosolsTermodinàmica atmosfèricaPollution010504 meteorology & atmospheric sciencesSingle-scattering albedomedia_common.quotation_subjectGeofísica010501 environmental sciencesRadiative forcingAtmospheric sciences01 natural sciencesPollutionAir pollution episodeAerosolAtmosphereBeijingRadiative transferEnvironmental ChemistryEnvironmental scienceAire Contaminació0105 earth and related environmental sciencesmedia_commonAerosol and Air Quality Research
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Brown Carbon Aerosol in Urban Xi'an, Northwest China: The Composition and Light Absorption Properties.

2018

Light-absorbing organic carbon (i.e., brown carbon or BrC) in the atmospheric aerosol has significant contribution to light absorption and radiative forcing. However, the link between BrC optical properties and chemical composition remains poorly constrained. In this study, we combine spectrophotometric measurements and chemical analyses of BrC samples collected from July 2008 to June 2009 in urban Xi'an, Northwest China. Elevated BrC was observed in winter (5 times higher than in summer), largely due to increased emissions from wintertime domestic biomass burning. The light absorption coefficient of methanol-soluble BrC at 365 nm (on average approximately twice that of water-soluble BrC) w…

Angstrom exponentChina010504 meteorology & atmospheric sciencesSOLUBLE ORGANIC-CARBONchemistry.chemical_element010501 environmental sciences01 natural sciencesEnvironmental ChemistryWATERPolycyclic Aromatic HydrocarbonsAbsorption (electromagnetic radiation)Chemical composition0105 earth and related environmental sciencesTotal organic carbonAerosolsAir PollutantsANGSTROM EXPONENTGeneral ChemistryCarbon blackOPTICAL-PROPERTIESRadiative forcingCarbonAerosolSOLAR-RADIATIONchemistrySOURCE APPORTIONMENTEnvironmental chemistryBLACK CARBONEnvironmental scienceFINE PARTICULATE MATTERSOUTHEASTERN UNITED-STATESCarbonBIOMASS-BURNING EMISSIONSEnvironmental sciencetechnology
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Air traffic and contrail changes during COVID-19 over Europe: A model study

2021

The strong reduction of air traffic during the COVID-19 pandemic provides a test case for the relation between air traffic density, contrails, and their radiative forcing of climate change. Air traffic and contrail cirrus changes are quantified for a European domain for March to August 2020 and compared to the same period in 2019. Traffic data show a 72 % reduction in flight distance compared with 2019. This paper investigates the induced contrail changes in a model study. The contrail model results depend on various methodological details tested in parameter studies. In the reference case, the reduced traffic caused an even stronger reduction in contrail length, partly because the w…

AtmosphereLongwaveEnvironmental scienceCirrusForcing (mathematics)Radiative forcingAtmospheric sciencesShortwaveWater vaporOptical depth
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Analysis of the aerosol radiative forcing over a Mediterranean urban coastal site

2014

Abstract The aerosol radiative forcing for the period 2003–2011 has been analyzed in Burjassot, Spain, an urban coastal site on the western Mediterranean, using measurements of global solar irradiance and aerosol properties, as well as simulated data. The aerosol radiative forcing was calculated at 5 minute intervals, and then integrated over 24 h to obtain daily mean values for 200 complete days under cloud-free skies. The monthly mean values of the aerosol radiative forcing showed a clear variation during the year, associated to the annual variability of the aerosol optical depth at 500 nm, ranging from − 6 to − 29 Wm− 2 at the surface, and from − 1.5 to − 3.9 Wm− 2 at the top of the atmo…

AtmosphereMediterranean climateCloud forcingAtmospheric ScienceAerosol radiative forcingClimatologyEnvironmental scienceRadiative forcingAbsorption (electromagnetic radiation)Solar irradianceAtmospheric sciencesAerosolAtmospheric Research
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