Search results for "Absorption"

showing 10 items of 2701 documents

The novel HALO mini-DOAS instrument: inferring trace gas concentrations from airborne UV/visible limb spectroscopy under all skies using the scaling …

2017

Abstract. We report on a novel six-channel optical spectrometer (further on called mini-DOAS instrument) for airborne nadir and limb measurements of atmospheric trace gases, liquid and solid water, and spectral radiances in the UV/vis and NIR spectral ranges. The spectrometer was developed for measurements from aboard the German High-Altitude and Long-Range (HALO) research aircraft during dedicated research missions. Here we report on the relevant instrumental details and the novel scaling method used to infer the mixing ratios of UV/vis absorbing trace gases from their absorption measured in limb geometry. The uncertainties of the scaling method are assessed in more detail than before for …

Atmospheric Science010504 meteorology & atmospheric sciences0207 environmental engineering02 engineering and technology010502 geochemistry & geophysics01 natural sciencesUV/visible limb spectroscopylaw.inventionOpticslawErdsystem-Modellierungddc:550Nadirlcsh:TA170-171020701 environmental engineeringAbsorption (electromagnetic radiation)SpectroscopyScaling0105 earth and related environmental sciencesRemote sensingSpectrometerVerkehrsmeteorologielcsh:TA715-787business.industrylcsh:Earthwork. FoundationsAtmosphärische SpurenstoffeOptical spectrometerlcsh:Environmental engineeringTrace gasHALO mini-DOASEarth sciences13. Climate actionEnvironmental scienceHalobusinessAtmospheric Measurement Techniques
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Multiyear in-situ measurements of atmospheric aerosol absorption properties at an urban coastal site in western Mediterranean

2016

Abstract In-situ aerosol absorption properties measured in Valencia (Spain) for four years, from February 2011 to February 2015, have been analysed. Spectral absorption properties have been obtained using a seven-wavelength Aethalometer AE-31 which covers the range from UV (370 nm) to IR (950 nm). In order to obtain the absorption coefficients, compensation parameters have been calculated for the Aethalometer considering seasonal and spectral differences. For this multiyear measurement period, seasonal site-specific calibration parameters have been obtained. Furthermore, estimations of the absorption Angstrom Exponent (α abs ) have been calculated using the seven Aethalometer wavelengths. T…

Atmospheric Science010504 meteorology & atmospheric sciencesChemistry010501 environmental sciencesSeasonalitymedicine.diseaseAethalometerAtmospheric sciences01 natural sciencesStandard deviationWavelengthBoundary layerClimatologyAttenuation coefficientmedicineCalibrationAbsorption (electromagnetic radiation)0105 earth and related environmental sciencesGeneral Environmental ScienceAtmospheric Environment
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Electron microscopy of particles collected at Praia, Cape Verde, during the Saharan Mineral Dust Experiment: particle chemistry, shape, mixing state …

2011

A large field experiment of the Saharan Mineral Dust Experiment (SAMUM) was performed in Praia, Cape Verde, in January and February 2008. The aerosol at Praia is a superposition of mineral dust, sea-salt, sulphates and soot. Particles smaller than 500 nm are mainly mineral dust, mineral dust–sulphate mixtures, sulphates and soot–sulphate mixtures. Particles larger then 2.5 μm consist of mineral dust, sea-salt and few mineral dust–sulphate mixtures. A transition range exists in between. The major internal mixtures are mineral dust–sulphate and soot–sulphate. Mineral dust–sea-salt mixtures occur occasionally, mineral dust–soot mixtures were not observed. The aspect ratio was 1.3–1.4 for dry p…

Atmospheric Science010504 meteorology & atmospheric sciencesChemistryMineralogy010501 environmental sciencesMineral dustmedicine.disease_causecomplex mixtures01 natural sciencesSootAerosolCape verdeAbsorption edgemedicineParticleParticle sizeAbsorption (electromagnetic radiation)0105 earth and related environmental sciencesTellus B: Chemical and Physical Meteorology
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Inter-comparison of stratospheric O<sub>3</sub> and NO<sub>2</sub> abundances retrieved from …

2006

Abstract. Stratospheric O3 and NO2 abundances measured by different remote sensing instruments are inter-compared: (1) Line-of-sight absorptions and vertical profiles inferred from solar spectra in the ultra-violet (UV), visible and infrared (IR) wavelength ranges measured by the LPMA/DOAS (Limb Profile Monitor of the Atmosphere/Differential Optical Absorption Spectroscopy) balloon payload during balloon ascent/descent and solar occultation are examined with respect to internal consistency. (2) The balloon borne stratospheric profiles of O3 and NO2 are compared to collocated space-borne skylight limb observations of the Envisat/SCIAMACHY satellite instrument. The trace gas profiles are retr…

Atmospheric Science010504 meteorology & atmospheric sciencesDifferential optical absorption spectroscopyBalloonAtmospheric sciences01 natural sciencesOccultationTrace gasSCIAMACHY010309 opticsAtmosphereAltitude13. Climate action0103 physical sciencesEnvironmental scienceSatellite0105 earth and related environmental sciencesRemote sensingAtmospheric Chemistry and Physics
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Evidence of ice crystals at cloud top of Arctic boundary-layer mixed-phase clouds derived from airborne remote sensing

2009

Abstract. The vertical distribution of ice crystals in Arctic boundary-layer mixed-phase (ABM) clouds was investigated by airborne remote-sensing and in situ measurements during the Arctic Study of Tropospheric Aerosol, Clouds and Radiation (ASTAR) campaign in March and April 2007. Information on the spectral absorption of solar radiation by ice and liquid water cloud particles is derived from airborne measurements of solar spectral radiation reflected by these clouds. It is shown by calculation of the vertical weighting function of the measurements that the observed absorption of solar radiation is dominated by the upper cloud layers (50% within 200 m from cloud top). This vertical weighti…

Atmospheric Science010504 meteorology & atmospheric sciencesIce crystalsBackscatterChemistryCloud topAtmospheric sciences01 natural sciencesPhysics::Geophysics010309 opticsBoundary layerArctic13. Climate actionLiquid water content0103 physical sciencesRadiative transferAbsorption (electromagnetic radiation)Astrophysics::Galaxy AstrophysicsPhysics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesRemote sensingAtmospheric Chemistry and Physics
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Black and brown carbon over central Amazonia: long-term aerosol measurements at the ATTO site

2018

The Amazon rainforest is a sensitive ecosystem experiencing the combined pressures of progressing deforestation and climate change. Its atmospheric conditions oscillate between biogenic and biomass burning (BB) dominated states. The Amazon further represents one of the few remaining continental places where the atmosphere approaches pristine conditions during occasional wet season episodes. The Amazon Tall Tower Observatory (ATTO) has been established in central Amazonia to investigate the complex interactions between the rainforest ecosystem and the atmosphere. Physical and chemical aerosol properties have been analyzed continuously since 2012. This paper provides an in-depth analysis of t…

Atmospheric Science010504 meteorology & atmospheric sciencesSingle-scattering albedoAmazon rainforest010501 environmental sciencesCombustionAtmospheric sciences01 natural scienceslcsh:QC1-999Aerosollcsh:ChemistryAtmospherelcsh:QD1-999Dry seasonForest ecologyEnvironmental scienceAbsorption (electromagnetic radiation)lcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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2016

Abstract. Scanning spectrometer networks using scattered solar radiation in the ultraviolet spectral region have become an increasingly important tool for monitoring volcanic sulfur dioxide (SO2) emissions. Often measured spectra are evaluated using the differential optical absorption spectroscopy (DOAS) technique. In order to obtain absolute column densities (CDs), the DOAS evaluation requires a Fraunhofer reference spectrum (FRS) that is free of absorption structures of the trace gas of interest. For measurements at volcanoes such a FRS can be readily obtained if the scan (i.e. series of measurements at different elevation angles) includes viewing directions where the plume is not seen. I…

Atmospheric Science010504 meteorology & atmospheric sciencesSpectrometerbusiness.industryDifferential optical absorption spectroscopy010502 geochemistry & geophysicsResidual01 natural sciencesSpectral lineTrace gasPlumeOpticsPrincipal component analysisEnvironmental sciencebusinessZenith0105 earth and related environmental sciencesRemote sensingAtmospheric Measurement Techniques
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Influence of clouds on the spectral actinic flux density in the lower troposphere (INSPECTRO): overview of the field campaigns

2008

Ultraviolet radiation is the key factor driving tropospheric photochemistry. It is strongly modulated by clouds and aerosols. A quantitative understanding of the radiation field and its effect on photochemistry is thus only possible with a detailed knowledge of the interaction between clouds and radiation. The overall objective of the project INSPECTRO was the characterization of the three-dimensional actinic radiation field under cloudy conditions. This was achieved during two measurement campaigns in Norfolk (East Anglia, UK) and Lower Bavaria (Germany) combining space-based, aircraft and ground-based measurements as well as simulations with the one-dimensional radiation transfer model UV…

Atmospheric ScienceAIRBORNEMODEL INTERCOMPARISON IPMMI010504 meteorology & atmospheric sciencesPHOTOCHEMICAL ACTIVITYmedia_common.quotation_subjectFluxPHOTOLYSIS FREQUENCY-MEASUREMENTRadiationAtmospheric sciences01 natural sciencesBROKEN CLOUDlaw.inventionTroposphere010309 opticslcsh:Chemistrylaw0103 physical sciencesddc:550MEASUREMENTSZenithABSORPTION CROSS-SECTIONSmedia_commonRemote sensingMonochromator0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereVERTICAL-DISTRIBUTIONStray lightlcsh:QC1-999UVJSpectroradiometerlcsh:QD1-999Sky13. Climate actionQUANTUM YIELDSEnvironmental science/dk/atira/pure/subjectarea/asjc/1900/1902lcsh:PhysicsAEROSOL EXTINCTION
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Contrast in column-integrated aerosol optical properties during heating and non-heating seasons at Urumqi — Its causes and implications

2017

Abstract Aerosol optical properties were retrieved from two years' worth of Sunphotometer measurements at Urumqi, an urban station in western China. Distinct seasonal variations of aerosol optical properties were revealed. During the heating season, mean aerosol optical depth at 550 nm (τ a ), Angstrom exponent calculated from aerosol optical depth at wavelength of 440 and 870 nm (α) as well as PM 2.5 concentration were 0.58 ± 0.33, 1.11 ± 0.34 and 79.5 ± 69.6 μg m − 3 , respectively, which contrasted their counterparts during the non-heating season of 0.32 ± 0.22, 0.79 ± 0.26, and 35.0 ± 20.1 μg m − 3 . Seasonal variations of τ a and PM 2.5 at Urumqi contrasted with corresponding values in…

Atmospheric ScienceAngstrom exponent010504 meteorology & atmospheric sciencesSingle-scattering albedo010501 environmental sciencesSeasonalityAtmospheric sciencesmedicine.disease01 natural sciencesAerosolWavelengthSpectroradiometermedicineEnvironmental scienceRelative humidityAbsorption (electromagnetic radiation)0105 earth and related environmental sciencesAtmospheric Research
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Determination and analysis of in situ spectral aerosol optical properties by a multi-instrumental approach

2014

Continuous in situ measurements of aerosol optical properties were conducted from 29 June to 29 July 2012 in Granada (Spain) with a seven-wavelength Aethalometer, a Multi-Angle Absorption Photometer, and a three-wavelength integrating nephelometer. The aim of this work is to describe a methodology to obtain the absorption coefficients (babs) for the different Aethalometer wavelengths. In this way, data have been compensated using algorithms which best estimate the compensation factors needed. Two empirical factors are used to infer the absorption coefficients from the Aethalometer measurements: C – the parameter describing the enhancement of absorption by particles in the filter matrix due …

Atmospheric ScienceAngstrom exponentAbsorption coefficientsMaterials science010504 meteorology & atmospheric sciencesAnalytical chemistry010501 environmental sciencesAethalometer01 natural sciencesGranada (Spain)Light scatteringlaw.inventionOpticslawlcsh:TA170-171Absorption (electromagnetic radiation)0105 earth and related environmental sciencesNephelometerlcsh:TA715-787business.industrylcsh:Earthwork. FoundationsAerosol optical propertiesPhotometerlcsh:Environmental engineeringAerosolWavelengthbusiness
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