Search results for "Dinàmica"

showing 10 items of 62 documents

Aerosol optical properties and direct radiative forcing based on measurements from the China Aerosol Remote Sensing Network (CARSNET) in eastern China

2018

Aerosol pollution in eastern China is an unfortunate consequence of the region's rapid economic and industrial growth. Here, sun photometer measurements from seven sites in the Yangtze River Delta (YRD) from 2011 to 2015 were used to characterize the climatology of aerosol microphysical and optical properties, calculate direct aerosol radiative forcing (DARF) and classify the aerosols based on size and absorption. Bimodal size distributions were found throughout the year, but larger volumes and effective radii of fine-mode particles occurred in June and September due to hygroscopic growth and/or cloud processing. Increases in the fine-mode particles in June and September caused AOD440 nm  &…

Termodinàmica atmosfèricaAtmospheric ScienceAngstrom exponent010504 meteorology & atmospheric sciencesSolar zenith angle010501 environmental sciencesMineral dustAtmospheric sciences01 natural scienceslcsh:ChemistrySun photometerAtmosphereSun photometer0105 earth and related environmental sciencesAerosolsRemote sensingRadiative forcinglcsh:QC1-999AerosolDirect aerosol radiative forcinglcsh:QD1-99913. Climate actionExtinction (optical mineralogy)Environmental sciencelcsh:PhysicsAerosol pollutionAtmospheric Chemistry and Physics
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Unexpected vertical structure of the Saharan Air Layer and giant dust particles during AER-D

2018

The Saharan Air Layer (SAL) in the summertime eastern Atlantic is typically well mixed and 3–4 km deep, overlying the marine boundary layer (MBL). In this paper, we show experimental evidence that at times a very different structure can be observed. During the AERosol properties – Dust (AER-D) airborne campaign in August 2015, the typical structure described above was observed most of the time, and was associated with a moderate dust content yielding an aerosol optical depth (AOD) of 0.3–0.4 at 355 nm. In an intense event, however, an unprecedented vertical structure was observed close to the eastern boundary of the basin, displaying an uneven vertical distribution and a very …

Termodinàmica atmosfèricaAtmospheric ScienceMarine boundary layerSaharan Air Layer010504 meteorology & atmospheric sciencesDust particles010502 geochemistry & geophysicsAtmospheric sciences01 natural scienceslcsh:ChemistryAtmosphereRadiative TransferRadiative transferDust transportGiant dust particlesAER-D0105 earth and related environmental sciencesSaharan Air LayerAerosol Optical DepthLightninglcsh:QC1-999Aerosollcsh:QD1-999Environmental scienceShortwavelcsh:PhysicsAtmospheric Chemistry and Physics
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Comparing different profiles to characterize the atmosphere for three MODIS TIR bands

2015

Abstract Accurate land surface temperature (LST) retrievals from sensors aboard orbiting satellites are dependent on the corresponding atmospheric correction, especially in the thermal infrared (TIR) spectral domain (8–14 μm). To remove the atmospheric effects from at-sensor measured radiance in the TIR range it is needed to characterize the atmosphere by means of three specific variables: the upwelling path and the hemispherical downwelling radiances plus the atmospheric transmissivity. Those variables can be derived from the previous knowledge of vertical atmospheric profiles of air temperature and relative humidity at different geo-potential heights and pressures. In this work, the above…

Termodinàmica atmosfèricaAtmospheric ScienceMean squared errorAtmospheric correctionSpectral bandsAtmospheric sciencesWeather stationAtmosphereAtmosferaDownwellingRadianceEnvironmental scienceRelative humidityRemote sensing
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A comparison of Microtops II and satellite ozone measurements in the period 2001-2011

2013

Daily average total ozone Microtops measurements obtained during several campaigns conducted from 2001 to 2011 at latitudes from 31 to 68N and in different seasons are compared with satellite observations. The Microtops ozone is derived using different wavelength combinations (Channel I, 305.5/312.5. nm; Channel II, 312.5/320. nm; and Channel III, 305.5/312.5/320. nm). Satellite data from TOMS, OMI, GOME, and GOME-2 are used in the comparison. The three Microtops channels show a high correlation with the satellite retrievals. Channel I shows the best results and produces a mean bias deviation (MBD) less than 2.14% with respect to TOMS, OMI and GOME. The MBD increases to 3% in the comparison…

Termodinàmica atmosfèricaAtmospheric ScienceOzoneOMIMicrotops II;OMI;TOMS;GOME;GOME-2;Total ozone contentMicrotops IITotal ozoneGeofísicaAtmospheric sciencesLatitudeTotal ozone contentWavelengthchemistry.chemical_compoundGOME-2GeophysicsTOMSchemistrySpace and Planetary ScienceSatellite dataEnvironmental scienceSatelliteGOMERemote sensingCommunication channel
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Retrieval of characteristic parameters for water vapour transmittance in the development of ground based Sun-Sky radiometric measurements of columnar…

2014

Abstract. Sun–sky radiometers are instruments created for aerosol study, but they can measure in the water vapour absorption band allowing the estimation of columnar water vapour in clear sky simultaneously with aerosol characteristics, with high temporal resolution. A new methodology is presented for estimating calibration parameters (i.e. characteristic parameters of the atmospheric transmittance and solar calibration constant) directly from the sun–sky radiometer measurements. The methodology is based on the hypothesis that characteristic parameters of the atmospheric transmittance are dependent on vertical profiles of pressure, temperature and moisture occurring at each site of measurem…

Termodinàmica atmosfèricaAtmospheric ScienceRadiometerMoisturelcsh:TA715-787Microwave radiometerlcsh:Earthwork. FoundationsSolar zenith angleCiències de la terraAerosollcsh:Environmental engineeringAtmosferaInfrared windowEnvironmental scienceRelative humiditylcsh:TA170-171Water vaporRemote sensing
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Precipitable water vapour content from ESR/SKYNET sun-sky radiometers: validation against GNSS/GPS and AERONET over three different sites in Europe

2018

The estimation of the precipitable water vapour content (W) with high temporal and spatial resolution is of great interest to both meteorological and climatological studies. Several methodologies based on remote sensing techniques have been recently developed in order to obtain accurate and frequent measurements of this atmospheric parameter. Among them, the relative low cost and easy deployment of sun–sky radiometers, or sun photometers, operating in several international networks, allowed the development of automatic estimations of W from these instruments with high temporal resolution. However, the great problem of this methodology is the estimation of the sun-photometric calibration par…

Termodinàmica atmosfèricaAtmospheric Scienceprecipitable water vapor; sun-sky radiometers; validation; GNSS/GPS010504 meteorology & atmospheric sciencesMeteorologyGPSprecipitable water vaporSolar zenith angleSKYNETAeronet01 natural sciences010309 opticsSkynet0103 physical sciencesCalibrationlcsh:TA170-1710105 earth and related environmental sciencesRemote sensingGNSS/GPS[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmospherevalidationPrecipitable waterbusiness.industrylcsh:TA715-787sun-sky radiometerslcsh:Earthwork. FoundationsAERONETlcsh:Environmental engineeringwater vapourGNSS applications13. Climate actionInfrared windowGlobal Positioning SystemEnvironmental sciencebusiness
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Coarse-mode mineral dust size distributions, composition and optical properties from AER-D aircraft measurements over the tropical eastern Atlantic

2018

Mineral dust is an important component of the climate system, affecting the radiation balance, cloud properties, biogeochemical cycles, regional circulation and precipitation, as well as having negative effects on aviation, solar energy generation and human health. Dust size and composition has an impact on all these processes. However, changes in dust size distribution and composition during transport, particularly for coarse particles, are poorly understood and poorly represented in climate models. Here we present new in situ airborne observations of dust in the Saharan Air Layer (SAL) and the marine boundary layer (MBL) at the beginning of its transatlantic transport pathway, from the AE…

Termodinàmica atmosfèrica[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere
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Física de l'atmòsfera: Lliçó 5. Equacions de moviment

2012

Aquesta lliçó forma part del curs de Física de l'Atmosfera del segon curs del Grau en Física. El tema desenvolupa les equacions de la dinàmica atmosfèrica (Navier-Stokes) i estableix les aproximacions bàsiques (aproximacions geostròfica, hidrostàtica i equacions de pronòstic)

UNESCO::CIENCIAS DE LA TIERRA Y DEL ESPACIO::Ciencias de la atmósfera ::Dinámica atmosféricafísicadinàmicaatmosfera
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Thermal-Infrared Spectral and Angular Characterization of Crude Oil and Seawater Emissivities for Oil Slick Identification

2014

Previous work has shown that the emissivity of crude oil is lower than that of the seawater in the thermal-infrared (TIR) spectrum. Thus, oil slicks cause an emissivity decrease relative to the seawater in that region. The aim of this paper was to carry out experimental measurements to characterize the spectral and angular variations of crude oil and seawater emissivities. The results showed that the crude oil emissivity is lower than the seawater emissivity and that it is essentially flat in the atmospheric window of 8-13 μm. The crude oil emissivity has a marked emissivity decrease with the angle (from 0.956 ± 0.005 at 15 ° to 0.873 ± 0.007 at 65 °), which is even higher than that of the …

Vessaments de petroliRadiometerCiències de la terraMineralogyRacing slickInfrared windowTermodinàmicaNadirEmissivityGeneral Earth and Planetary SciencesEnvironmental scienceRadiometrySatelliteSeawaterElectrical and Electronic EngineeringRemote sensingIEEE Transactions on Geoscience and Remote Sensing
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La historia del primer principio de la termodinámica y sus implicaciones didácticas

2007

En este trabajo se realiza una breve introduccion historica y epistemologica del nacimiento de la termodinamica como ciencia moderna. Se muestra, asi mismo, como esta historia puede contribuir a mejorar la ensenanza de la termodinamica y a superar algunas dificultades de los estudiantes.Palabras Clave: historia de la ciencia; ensenanza y aprendizaje de la termodinamicaThe history of the first law of thermodynamics and its didactict implicationsIn this work is carried out a brief historical and epistemological introduction of the thermodynamics’ birth as a modern science. It is shown, likewise, how this history can contribute to improve the teaching of thermodynamics and to overcome some stu…

historia de la cienciaCiències físiquesPhilosophySocial Sciencesenseñanza y aprendizaje de la termodinámicaEducationlcsh:Social Scienceslcsh:HHTermodinàmicaEducacióHistory of scienceHumanitiesEnsenyamentRevista Eureka sobre enseñanza y divulgación de las ciencias.
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