Search results for "IR M"

showing 10 items of 151 documents

Columnar aerosol properties in a Northeastern Atlantic site (Plymouth, United Kingdom) by means of ground based skyradiometer data during years 2000-…

2012

Between 2000 and 2008, columnar optical and radiative properties were measured at the Plymouth Marine Laboratory (PML), UK (50° 21.95'N, 4° 8.85'W) using an automatic Prede POM01L sun-sky photometer. The database was analyzed for aerosol optical properties using the SKYRAD radiative inversion algorithm and calibrated using the in situ SKYIL calibration method. Retrievals include aerosol optical depth, ångström wavelength exponent, aerosol volume distribution, refractive index and single scattering albedo. The results show that the Plymouth site is characterized by low values of aerosol optical depth with low variability (0.18 ± 0.08 at 500 nm) and a mean annual ångström exponent of 1.03 ± 0…

Atmospheric ScienceAngstrom exponentSKYNETSingle-scattering albedoMarine aerosolsSKYNETAODMineral dustAerosolWavelengthSkyradiometerClimatologyRadiative transferPrede POMAir massGeneral Environmental ScienceESR
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Influence of air mass history on the columnar aerosol properties at Valencia, Spain

2007

[1] The physical and radiative properties of atmospheric aerosols have been obtained in Valencia (latitude 39.508°, longitude −0.418°, 60 m a. s. l.), a city of the Spanish Mediterranean coast, by the inversion of direct solar irradiance and diffuse sky irradiance measurements made with a CIMEL CE318 system, from January 2002 to July 2005. The data acquired by the CE318 were used to determine the instantaneous values of the aerosol optical depth (AOD), the columnar water vapor content (w) and the Angstrom wavelength exponent (α). The SKYRAD code was used to obtain the size distribution, the asymmetry parameter, the complex refractive index and the single scattering albedo of the aerosols. B…

Atmospheric ScienceEcologyMeteorologySingle-scattering albedoIrradiancePaleontologySoil ScienceForestryAquatic ScienceOceanographySolar irradianceAtmospheric sciencesAerosolGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Radiative transferEnvironmental scienceLongitudeWater vaporAir massEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Climatology of convective density currents in the southern foothills of the Atlas Mountains

2010

Density currents fed by evaporationally cooled air are an important dust storm generating feature and can constitute a source of moisture in arid regions. Recently, the existence of such systems has been demonstrated for the area between the High Atlas Mountains and the Sahara desert in southern Morocco on the basis of case studies. Here, a climatological analysis is presented that uses data from the dense climate station network of the IMPETUS project (An Integrated Approach to the Efficient Management of Scarce Water Resources in West Africa) for the 5 year period 20022006. Objective criteria mainly based upon abrupt changes in wind and dew point temperature are defined to identify possib…

Atmospheric ScienceEcologyPaleontologySoil ScienceForestryAquatic ScienceOceanographyAtmospheric temperatureAridWind speedAtmosphereGeophysicsDew pointSpace and Planetary ScienceGeochemistry and PetrologyDust stormDiurnal cycleClimatologyEarth and Planetary Sciences (miscellaneous)Environmental scienceAir massEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Altitude effect in UV radiation during the Evaluation of the Effects of Elevation and Aerosols on the Ultraviolet Radiation 2002 (VELETA-2002) field …

2008

[1] The Evaluation of the Effects of Elevation and Aerosols on the Ultraviolet Radiation 2002 (VELETA-2002) field campaign was designed to study the influence of aerosols and altitude on solar UV irradiance. The altitude effect (AE) was evaluated for UV irradiance under cloudless conditions by taking spectral and broadband measurements in SE Spain in the summer of 2002 at three nearby sites located at different heights (680 m, 2200 m, and 3398 m). A spectral radiative transfer model (Santa Barbara DISORT Atmospheric Radiative Transfer (SBDART)) was also applied, mainly to evaluate the tropospheric ozone impact on AE. Results are related to the optical properties and air mass origin of the a…

Atmospheric ScienceEcologySolar zenith angleIrradiancePaleontologySoil ScienceForestryAquatic ScienceMineral dustNoonOceanographyAtmospheric scienceschemistry.chemical_compoundGeophysicsAltitudeAtmospheric radiative transfer codeschemistrySpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Environmental scienceTropospheric ozoneAir massEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Effect of variation of the vertical air density profile on the relative optical air mass

1967

A simple method is developed which allows for estimating the deviations of the relative optical air mass for a given vertical air density profile from the relative optical air mass for the ARDC Model Atmosphere, 1959 which serves as standard. In case of the mean profiles given byQuiroz [3] for middle latitudes, summer; middle latitudes, winter; arctic summer; and arctic winter the air mass deviations turn out to be small.

Atmospheric ScienceGeneral MedicineAtmospheric sciencesPhysics::GeophysicsAtmosphereArcticClimatologyMiddle latitudesPhysics::Space PhysicsEnvironmental scienceDensity of airVariation (astronomy)Physics::Atmospheric and Oceanic PhysicsAir massEarth-Surface ProcessesArchiv für Meteorologie, Geophysik und Bioklimatologie Serie B
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Sampling of an STT event over the Eastern Mediterranean region by lidar and electrochemical sonde

2005

A two-wavelength ultraviolet (289–316nm) ozone Differential Absorption Lidar (DIAL) system is used to perform ozone measurements in the free troposphere in the Eastern Mediterranean (Northern Greece). The ozone DIAL profiles obtained during a Stratosphere-to-Troposphere Transport (STT) event are compared to that acquired by an electrochemical ozonesonde, in the altitude range between 2 and 10 km. The measurement accuracy of these two instruments is also discussed. The mean difference between the ozone profiles obtained by the two techniques is of the order of 1.11 ppbv (1.86%), while the corresponding standard deviation is 4.69 ppbv (8.16%). A case study of an STT event which occurred on 29…

Atmospheric ScienceOzone010504 meteorology & atmospheric sciencesMeteorology[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010501 environmental sciencesAtmospheric sciences01 natural sciencesTroposphereAtmospherechemistry.chemical_compoundPotential vorticityEarth and Planetary Sciences (miscellaneous)Mixing ratiolcsh:ScienceStratosphereAir mass0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere[SDU.OCEAN] Sciences of the Universe [physics]/Ocean Atmospherelcsh:QC801-809GeologyAstronomy and Astrophysicslcsh:QC1-999lcsh:Geophysics. Cosmic physicsLidarchemistry13. Climate actionSpace and Planetary Science[SDU.STU] Sciences of the Universe [physics]/Earth SciencesEnvironmental sciencelcsh:Qlcsh:Physics
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A complex case study of down to the surface intrusions of persistent stratospheric air over the Eastern Mediterranean

2006

Abstract In this study, we present a complex case study of concurrent stratosphere-to-troposphere transport (STT) events down to the surface of a low topography region in Northern Greece, which occurred in spring 2000. Two surface stations at Livadi (850 m asl) and Thessaloniki (20 m asl) were influenced by intrusions of stratospheric air masses that persisted for a time period from 7 to 10 days within the troposphere before reaching the stations. Before reaching the surface stations in Greece, the air masses crossed the tropopause in different synoptic systems over Eastern Europe, N. America and the N. Atlantic. This is the first study, to our knowledge, that presents a down to the surface…

Atmospheric ScienceOzoneAtmospheric circulationMediterranean BasinTropospherechemistry.chemical_compoundchemistryPotential vorticityClimatologyEnvironmental scienceTropopauseStratosphereAir massGeneral Environmental ScienceAtmospheric Environment
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2012

Abstract. Measurements of the ambient aerosol were performed at the Southern coast of Spain, within the framework of the DOMINO (Diel Oxidant Mechanisms In relation to Nitrogen Oxides) project. The field campaign took place from 20 November until 9 December 2008 at the atmospheric research station "El Arenosillo" (37°5'47.76" N, 6°44'6.94" W). As the monitoring station is located at the interface between a natural park, industrial cities (Huelva, Seville) and the Atlantic Ocean, a variety of physical and chemical parameters of aerosols and gas phase could be characterized in dependency on the origin of air masses. Backwards trajectories were examined and compared with local meteorology to c…

Atmospheric ScienceOzoneAtmospheric sciencesMass spectrometryAerosolTrace gaschemistry.chemical_compoundchemistryClimatologyParticleEnvironmental scienceSulfateChemical compositionAir massAtmospheric Chemistry and Physics
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Organic and inorganic bromine measurements around the extratropical tropopause and lowermost stratosphere: insights into the transport pathways and t…

2021

We report on measurements of total bromine (Brtot) in the upper troposphere and lower stratosphere taken during 15 flights with the German High Altitude and LOng range research aircraft (HALO). The research campaign WISE (Wave-driven ISentropic Exchange) included regions over the North Atlantic, Norwegian Sea, and northwestern Europe in fall 2017. Brtot is calculated from measured total organic bromine (Brorg) added to inorganic bromine (Bryinorg), evaluated from measured BrO and photochemical modeling. Combining these data, the weighted mean [Brtot] is 19.2±1.2 ppt in the northern hemispheric lower stratosphere (LS), in agreement with expectations for Brtot in the middle stratosphere (Enge…

Atmospheric SciencePhysicsQC1-999Radiative forcingAtmospheric sciencesTrace gasTroposphereEarth sciencesChemistryMiddle latitudesddc:550Environmental scienceEast Asian MonsoonTropopauseStratosphereQD1-999Air massAtmospheric Chemistry and Physics
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Column-integrated aerosol optical properties in Sodankylä (Finland) during the Solar Induced Fluorescence Experiment (SIFLEX-2002).

2006

[1] A study has been made of the column aerosols using solar irradiance extinction measurements at ground level in a boreal region (Sodankyla, Finland) during spring 2002. The aerosol properties have been related to air mass origin. In general, the aerosol levels were observed to be very low, independent of the air mass origin, with an aerosol optical depth (AOD) value at 500 nm of less than 0.09 ± 0.03. Two characteristic patterns were observed depending on whether the air masses originated in the north and west or from the south and east. In the first case (north and west origins) the aerosol load was very small, with very low optical depths in the range 0.03 ± 0.02 to 0.09 ± 0.03 for 500…

Atmospheric ScienceRadiació solarMeteorologySoil ScienceAquatic ScienceOceanographySolar irradianceAtmospheric sciencesGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Air massEarth-Surface ProcessesWater Science and TechnologyAerosolsEcologySpring seasonPaleontologyForestryGeofísicaAerosolGround levelWavelengthGeophysicsBorealSpace and Planetary ScienceExtinction (optical mineralogy)Environmental science
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