Bibliografías temáticas / Aerosols – Optical properties

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Literatura académica sobre el tema "Aerosols – Optical properties"

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Publicado: 4 de junio de 2021
Última modificación: 6 de septiembre de 2023

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Artículos de revistas sobre el tema "Aerosols – Optical properties"

1

Zhuang, Bingliang, Tijian Wang, Jane Liu, et al. "The optical properties, physical properties and direct radiative forcing of urban columnar aerosols in the Yangtze River Delta, China." Atmospheric Chemistry and Physics 18, no. 2 (2018): 1419–36. http://dx.doi.org/10.5194/acp-18-1419-2018.

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Abstract. The optical and physical properties as well as the direct radiative forcings (DRFs) of fractionated aerosols in the urban area of the western Yangtze River Delta (YRD) are investigated with measurements from a Cimel sun photometer combined with a radiation transfer model. Ground-based observations of aerosols have much higher temporal resolutions than satellite retrievals. An initial analysis reveals the characteristics of the optical properties of different types of fractionated aerosols in the western YRD. The total aerosols, mostly composed of scattering components (93.8 %), have
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Pedrós, R., J. L. Gómez-Amo, C. R. Marcos, et al. "AEROgui: A Graphical User Interface for the Optical Properties of Aerosols." Bulletin of the American Meteorological Society 95, no. 12 (2014): 1863–71. http://dx.doi.org/10.1175/bams-d-13-00162.1.

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Atmospheric aerosols have an uncertain effect on climate and serious impacts on human health. The uncertainty in the aerosols' role on climate has several sources. First, aerosols have great spatial and temporal variability. The spatial variability arises from the fact that aerosols emitted in a certain place can travel thousands of kilometers, swept by the winds to modify the destination region's climate. The spatial variability also means that aerosols are inhomogeneously distributed in the vertical direction, which can lead to a differential effect on the energy balance depending on the aer
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Peers, F., F. Waquet, C. Cornet, et al. "Absorption of aerosols above clouds from POLDER/PARASOL measurements and estimation of their direct radiative effect." Atmospheric Chemistry and Physics 15, no. 8 (2015): 4179–96. http://dx.doi.org/10.5194/acp-15-4179-2015.

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Abstract. This study presents an original method to evaluate key parameters for the estimation of the direct radiative effect (DRE) of aerosol above clouds: the absorption of the the cloud albedo. It is based on multi-angle total and polarized radiances both provided by the A-train satellite instrument POLDER – Polarization and Directionality of Earth Reflectances. The sensitivities brought by each kind of measurements are used in a complementary way. Polarization mostly translates scattering processes and is thus used to estimate scattering aerosol optical thickness and aerosol size. On the o
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4

Abd Jalal, Khairunnisa, Arnis Asmat, and Noordin Ahmad. "Retrievals of Aerosol Optical Depth and Angstrom Exponent for Identification of Aerosols at Kuching, Sarawak." Advanced Materials Research 518-523 (May 2012): 5734–37. http://dx.doi.org/10.4028/www.scientific.net/amr.518-523.5734.

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Anthropogenic and natural aerosols are important atmospheric constituents that significantly contribute to the Earth’s radiation budget but remain uncertainties due to the poor understanding of aerosol properties and its direct effects on scattering and absoprtion of solar radiation and the ability of aerosols to stay in atmosphere for a very short time. Different types of aerosols, representing biomass burning, urban or continental aerosols, maritime aerosols and dust particles will give different characterization and classification of aerosol properties. The data used in this study was obtai
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Bergstrom, R. W., P. Pilewskie, P. B. Russell, et al. "Spectral absorption properties of atmospheric aerosols." Atmospheric Chemistry and Physics 7, no. 23 (2007): 5937–43. http://dx.doi.org/10.5194/acp-7-5937-2007.

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Abstract. We have determined the solar spectral absorption optical depth of atmospheric aerosols for specific case studies during several field programs (three cases have been reported previously; two are new results). We combined airborne measurements of the solar net radiant flux density and the aerosol optical depth with a detailed radiative transfer model for all but one of the cases. The field programs (SAFARI 2000, ACE Asia, PRIDE, TARFOX, INTEX-A) contained aerosols representing the major absorbing aerosol types: pollution, biomass burning, desert dust and mixtures. In all cases the spe
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Peers, F., F. Waquet, C. Cornet, et al. "Absorption of aerosols above clouds from POLDER/PARASOL measurements and estimation of their Direct Radiative Effect." Atmospheric Chemistry and Physics Discussions 14, no. 18 (2014): 25533–79. http://dx.doi.org/10.5194/acpd-14-25533-2014.

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Abstract. The albedo of clouds and the aerosol absorption are key parameters to evaluate the direct radiative effect of an aerosol layer above clouds. While most of the retrievals of above clouds aerosol characteristics rely on assumptions on the aerosol properties, this study offers a new method to evaluate aerosol and cloud optical properties simultaneously (i.e. aerosol and cloud optical thickness, aerosol single scattering albedo and angström exponent). It is based on multi-angle total and polarized radiances both provided by the A-train satellite instrument POLDER – Polarization and Direc
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7

Jung, Chang Hoon, Sang Hee Han, Ji Yi Lee, and Yong Pyo Kim. "Source-Based Size-Resolved Optical Properties of Carbonaceous Aerosols." Applied Sciences 11, no. 4 (2021): 1434. http://dx.doi.org/10.3390/app11041434.

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In this study, the source-based optical properties of polydisperse carbonaceous aerosols were determined from PM2.5 concentrations measured at a Global Atmospheric Watch station in South Korea. The extinction and absorption coefficients of carbonaceous aerosols were calculated using the Mie theory and assuming a lognormal size distribution. Based on the mass concentration from the EPA’s Positive Matrix Factorization (PMF) receptor model, which considers five source identification and apportionment factors (biogenic source, local biomass burning, secondary organic aerosol, transported biomass b
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Bergstrom, R. W., P. Pilewskie, P. B. Russell, et al. "Spectral absorption properties of atmospheric aerosols." Atmospheric Chemistry and Physics Discussions 7, no. 4 (2007): 10669–86. http://dx.doi.org/10.5194/acpd-7-10669-2007.

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Abstract. We have determined the solar spectral absorption optical depth of atmospheric aerosols for specific case studies during several field programs (three cases have been reported previously; two are new results). We combined airborne measurements of the solar net radiant flux density and the aerosol optical depth with a detailed radiative transfer model for all but one of the cases. The field programs (SAFARI 2000, ACE Asia, PRIDE, TARFOX, INTEX-A) contained aerosols representing the major absorbing aerosol types: pollution, biomass burning, desert dust and mixtures. In all cases the spe
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9

Sapkota, Santosh, Sabin Gautam, Santosh Pokhrel, et al. "Study of aerosol optical properties in Lumbini, Nepal." BIBECHANA 20, no. 1 (2023): 1–9. http://dx.doi.org/10.3126/bibechana.v20i1.48825.

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The mixture of different sized particles (fine and coarse) with air composition forms aerosols. Increased economic activities, vehicles, and rapid urbanization made Lumbini one of the heavily polluted regions in Nepal. Data are extracted from AERONET websites between 2013 to 2019 with standard deviation. We are mainly focused on understanding variations in aerosol optical properties: aerosol optical depth (AOD), angstrom parameter (α and β), visibility, single-scattering albedo (SSA), refractive index (real and imaginary), and asymmetry parameter (AP) in the Lumbini region. The maximum value o
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Tang, Yanxia, Yong Huang, and Keyong Zhu. "Optical Properties of Black Carbon Aerosols with Different Coating Models." Photonics 9, no. 5 (2022): 359. http://dx.doi.org/10.3390/photonics9050359.

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Research on the optical properties of black carbon (BC) aerosols is highly important for investigating global climate change. A general inhomogeneous particle superposition model is developed. Inhomogeneous particles with arbitrary shapes can be constructed by this model. BC aerosols with core-shell, spherical, ellipsoid, and irregular coating models are established to explore the impact of coating shape on their optical properties. The optical properties are studied employing the discrete dipole approximation method (DDA). The influences of the morphology of BC aerosols, the coating volume fr
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Tesis sobre el tema "Aerosols – Optical properties"

1

Laucks, Mary Lisa. "Quantifying the uncertainties in measurements of aerosol optical properties relevant to the direct shortwave forcing of climate /." Thesis, Connect to this title online; UW restricted, 1996. http://hdl.handle.net/1773/10314.

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Farino, John. "Influence of aerosol properties on signals and interferences in optical atomic spectrometry." Diss., Georgia Institute of Technology, 1985. http://hdl.handle.net/1853/30009.

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Zhang, Dan. "Laboratory investigation of chemical and physical properties of soot-containing aerosols." Texas A&M University, 2003. http://hdl.handle.net/1969.1/3977.

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Soot particles released from fossil fuel combustion and biomass burning have a large impact on the regional/global climate by altering the atmospheric radiative properties and by serving as cloud condensation nuclei (CCN). However, the exact forcing is affected by the mixing of soot with other aerosol constituents, such as sulfuric acid. In this work, experimental studies have been carried out focusing on three integral parts: (1) heterogeneous uptake of sulfuric acid on soot; (2) hygroscopic growth of H2SO4-coated soot aerosols; (3) effect of H2SO4 coating on scattering and extinction propert
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Ripoll, Roca Anna. "Physical, optical and chemical properties of atmospheric aerosols in the western Mediterranean continental background." Doctoral thesis, Universitat de Barcelona, 2015. http://hdl.handle.net/10803/305999.

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Atmospheric aerosols have played a key role in the development of the Earth’s atmosphere. Without atmospheric particles rainfall would be nonexistent and the climate would be very different. However, anthropogenic emissions have changed the chemical composition of atmospheric aerosols significantly through emissions of particles and precursor gases, particularly since the industrial revolution. Moreover, numerous studies have demonstrated that atmospheric aerosols, both natural and anthropogenic, do not only influence Earth’s climate, but also have adverse effects on human health, ecosystems,
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Yeung, Ming Chee. "Study of phase transition and hygroscopic properties of pure and multi-component atmospheric particles by optical microscopic imaging and micro-raman spectroscopy /." View abstract or full-text, 2009. http://library.ust.hk/cgi/db/thesis.pl?EVNG%202009%20YEUNG.

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Zhu, Xijing. "Investigation of Aerosol Optical and Chemical Properties Using Humidity Controlled Cavity Ring-Down Spectroscopy." PDXScholar, 2017. https://pdxscholar.library.pdx.edu/open_access_etds/4032.

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Scientists have been observing a change in the climate since the beginning of the 20th century that cannot be attributed to any of the natural influences of the past. Natural and anthropogenic substances and processes perturb the Earth's energy budget, contributing to climate change. In particular, aerosols (particles suspended in air) have long been recognized to be important in processes throughout the atmosphere that affect climate. They directly influence the radiative balance of the Earth's atmosphere, affect cloud formation and properties, and are also key air pollutants that contribute
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Liu, Jiumeng. "Chemical and optical properties of organic aerosols in the atmosphere over continental US: formation, partitioning, and light absorption." Diss., Georgia Institute of Technology, 2013. http://hdl.handle.net/1853/50370.

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The chemical and optical properties of particulate organic compounds remain unclear, which leaves large uncertainties in the estimation of global radiative transfer balance. Gas and find particle (PM2.5) phase formic acid concentrations were measured with online instrumentation during separate one-month studies in the summer of 2010 in Los Angeles (LA), CA, and Atlanta, GA, and the gas-particle partitioning behavior was investigated and compared with that of water-soluble organic compounds (WSOC). The diurnal profiles clearly indicated that the photochemistry production serves as a strong sour
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8

Rawle, Christopher B., and n/a. "Coherent multiwavelength sources for tropospheric aerosol lidar." University of Otago. Department of Physics, 2005. http://adt.otago.ac.nz./public/adt-NZDU20070427.114533.

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The monitoring and study of the earth�s atmosphere is becoming an increasingly important task given the current uncertainties in climate prediction. Areas where lidar has been used to further understanding of the atmosphere include monitoring of greenhouse gases, global warming, stratospheric ozone depletion, photochemical smog and aerosol photochemistry. However, the potentially severe long term effects of anthropogenic aerosols on earth�s biosphere are poorly understood. This project seeks to apply state of the art laser technology to develop an innovative multiwavelength lidar system capabl
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9

COSTA, RENATA F. da. "Estudo das propriedades opticas dos aerossois no estado de Sao Paulo com a tecnica de Lidar Raman." reponame:Repositório Institucional do IPEN, 2010. http://repositorio.ipen.br:8080/xmlui/handle/123456789/9586.

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Made available in DSpace on 2014-10-09T12:28:19Z (GMT). No. of bitstreams: 0<br>Made available in DSpace on 2014-10-09T13:56:45Z (GMT). No. of bitstreams: 0<br>Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)<br>Dissertacao (Mestrado)<br>IPEN/D<br>Instituto de Pesquisas Energeticas e Nucleares - IPEN-CNEN/SP<br>FAPESP:08/01954-0
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SOUZA, RENATA F. de. "Estudo do perfil vertical de aerossóis na troposfera utilizando a técnica de LIDAR." reponame:Repositório Institucional do IPEN, 2004. http://repositorio.ipen.br:8080/xmlui/handle/123456789/9294.

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Made available in DSpace on 2014-10-09T12:25:48Z (GMT). No. of bitstreams: 0<br>Made available in DSpace on 2014-10-09T14:03:33Z (GMT). No. of bitstreams: 1 11315.pdf: 4284842 bytes, checksum: 94ad34802b7652ff6ef2b3584c12f794 (MD5)<br>Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)<br>Dissertacao (Mestrado)<br>IPEN/D<br>Instituto de Pesquisas Energeticas e Nucleares, IPEN/CNEN-SP<br>FAPESP:01/07304-8
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Libros sobre el tema "Aerosols – Optical properties"

1

Nagel, Dagmar. Analyse der optischen Eigenschaften des arktischen Aerosols =: Analysis of optical properties of Arctic aerosol. Alfred-Wegener-Institut für Polar- und Meeresforschung, 1999.

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G, Zvenigorodskiĭ S., та Komarov V. S. 1932-, ред. Opticheskai͡a︡ modelʹ sredneĭ atmosfery. "Nauka," Sibirskoe otd-nie, 1990.

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Ivlev, L. S. Opticheskie svoĭstva atmosfernykh aėrozoleĭ. Izd-vo Leningradskogo universiteta, 1986.

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E, Zuev V., Kopytin I͡U︡ D, and Institut optiki atmosfery (Akademii͡a︡ nauk SSSR), eds. Opticheskiĭ razri͡a︡d v aėrozoli͡a︡kh. "Nauka," Sibirskoe otd-nie, 1990.

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Zuev, V. E. Optika atmosfernogo aėrozoli͡a︡. Gidrometeoizdat, 1987.

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Ivlev, L. S. Opticheskie svoĭstva atmosfernykh aėrozoleĭ. Izd-vo Leningradskogo universiteta, 1986.

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D, Kopytin I͡U︡, Belan B. D та Institut optiki atmosfery (Akademii͡a︡ nauk SSSR), ред. Prostranstvennai͡a︡ izmenchivostʹ kharakteristik atmosfernogo aėrozoli͡a︡. "Nauka," Sibirskoe otd-nie, 1989.

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Takemura, Toshihiko. A study on aerosol distributions and optical properties with a global climate model. University of Tokyo, Center for Climate System Research, 2002.

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Takemura, Toshihiko. A study on aerosol distributions and optical properties with a global climate model. University of Tokyo, Center for Climate System Research, 2002.

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Tōkyō Daigaku. Kikō Shisutemu Kenkyū Sentā, ed. A study on aerosol distributions and optical properties with a global climate model. University of Tokyo, Center for Climate System Research, 2002.

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Capítulos de libros sobre el tema "Aerosols – Optical properties"

1

Boucher, Olivier. "Physical, Chemical and Optical Aerosol Properties." In Atmospheric Aerosols. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9649-1_3.

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Hasan, F. M., and I. Sabbah. "Variations of Desert Dust Optical Properties over Solar Village, KSA." In Nucleation and Atmospheric Aerosols. Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-6475-3_228.

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Hasan, F. M., and I. Sabbah. "Atmospheric Aerosols Optical Properties and Climate over Solar Village, KSA." In Nucleation and Atmospheric Aerosols. Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-6475-3_229.

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Saha, Auromeet, Marc Mallet, Jean Claude Roger, Philippe Dubuisson, Jacques Piazzola, and Serge Despiau. "Optical Properties and Radiative Effects of Aerosols in a Coastal Zone." In Nucleation and Atmospheric Aerosols. Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-6475-3_138.

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Chow, Judith, John Watson, Douglas Lowenthal, and Nehzat Motallebi. "Measurement of Ultrafine and Fine Particle Black Carbon and its Optical Properties." In Nucleation and Atmospheric Aerosols. Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-6475-3_134.

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Pilinis, Christodoulos, and Spyros N. Pandis. "Physical, Chemical and Optical Properties of Atmospheric Aerosols." In Airborne Particulate Matter. Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-540-49145-3_4.

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Cheng, Y. F., Alfred Wiedensohler, H. Eichler, et al. "Relative Humidity Dependence of Aerosol Optical Properties and Direct Radiative Forcing in the Surface Boundary Layer of Southeastern China." In Nucleation and Atmospheric Aerosols. Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-6475-3_96.

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Moon, Kwang-Joo, Jin-Seok Han, and Yoo-Duck Hong. "Physical, Chemical and Optical Properties of Fine Aerosol as a Function of Relative Humidity at Gosan, Korea during ABC-EAREX 2005." In Nucleation and Atmospheric Aerosols. Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-6475-3_198.

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Urbanski, Shawn P., Susan M. O’Neill, Amara L. Holder, Sarah A. Green, and Rick L. Graw. "Emissions." In Wildland Fire Smoke in the United States. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-87045-4_5.

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AbstractThis chapter assesses the current state of the science regarding the composition, intensity, and drivers of wildland fire emissions in the USA and Canada. Globally and in the USA wildland fires are a major source of gases and aerosols which have significant air quality impacts and climate interactions. Wildland fire smoke can trigger severe pollution episodes with substantial effects on public health. Fire emissions can degrade air quality at considerable distances downwind, hampering efforts by air regulators to meet air standards. Fires are a major global source of aerosols which affect the climate system by absorbing and scattering radiation and by altering optical properties, coverage, and lifetime of clouds. A thorough understanding of fire emissions is essential for effectively addressing societal and climate consequences of wildland fire smoke.
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Paraskevopoulou, D., E. Gerasopoulos, E. Liakakou, et al. "Optical Properties of Aerosols Over Athens, Greece, and Their Relation with Chemical Composition." In Advances in Meteorology, Climatology and Atmospheric Physics. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29172-2_162.

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Actas de conferencias sobre el tema "Aerosols – Optical properties"

1

Egan, Walter G. "Infrared optical properties of atmospheric aerosols." In OSA Annual Meeting. Optica Publishing Group, 1985. http://dx.doi.org/10.1364/oam.1985.fp3.

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The infrared optical properties of atmospheric aerosols can strongly affect the radiative transfer properties of the atmosphere. One past method for determining the transmission properties of aerosols depended on measurements on potassium bromide pellets (containing the aerosols) on an infrared spectrophotometer. However, for some materials there is a discrepancy between measurements made with a laser source and those made with a spectrophotometer; but for other materials there is good agreement. The reason for the disagreement appears to be in the resolution of the measurement. Typically, a P
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Ferrare, R. A., S. H. Melfi, D. N. Whiteman, and K. D. Evans. "Coincident Measurements of Atmospheric Aerosol Properties and Water Vapor by a Scanning Raman Lidar." In Optical Remote Sensing of the Atmosphere. Optica Publishing Group, 1993. http://dx.doi.org/10.1364/orsa.1993.mb.2.

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Knowledge of the physical and optical properties of atmospheric aerosols is required to determine the impact aerosols will have on radiative transfer, heterogeneous chemistry, and cloud dynamics. Since the composition and size of atmospheric aerosols are functions of the atmospheric water vapor, aerosols must be studied in their natural state in order to fully understand how they are affected by various meteorological conditions and how they in turn will affect the processes listed above. By measuring high resolution profiles of aerosol extinction and backscattering as well as simultaneous pro
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Grant, William B., Edward V. Browell, Bruce E. Anderson, and Syed Ismail. "Airborne Lidar Measurements of Aerosols." In Optical Remote Sensing of the Atmosphere. Optica Publishing Group, 1993. http://dx.doi.org/10.1364/orsa.1993.tha.4.

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Aerosols are now recognized as having a significant impact on global climate. Aerosols affect climate directly via scattering and absorption, and indirectly through their effect on cloud properties, generally acting in a manner that counteracts the warming induced by greenhouse gases such as CO2[Charlson et al., 1992; Fouquart and Isaka, 1992; Penner et al., 1992]. The NASA Langley Research Center's airborne UV DIAL system measures vertical-profile of aerosol scattering at IR, visible, and UV wavelengths at distances up to 25 km above and 12 km below the aircraft. The system has been operated
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Sano, Itaru, Sonoyo Mukai, and Tsutomu Takashima. "Polarimetric properties of atmospheric aerosols." In Optical Science, Engineering and Instrumentation '97. SPIE, 1997. http://dx.doi.org/10.1117/12.278981.

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Chu, W. P. "Estimation of aerosol optical properties from the Inversion of extinction measurements." In OSA Annual Meeting. Optica Publishing Group, 1988. http://dx.doi.org/10.1364/oam.1988.ww1.

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This paper deals with the problem of estimating the optical properties of aerosols based on a finite number of extinction measurements. This kind of problem arises in many situations involving the remote sensing of aerosols with optical instrumentation such as radiometers for extinction measurements and lidar systems for backscattering measurements. A technique has been developed so that extinction measurements at a finite number of spectral regions can be inverted directly to yield either extinction or backscattering values at other wavelength regions without solving for the aerosol size dist
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Voss, Kenneth, and Yi Liu. "Polarized radiance distribution measurements of skylight for passive remote sensing of aerosol optical properties." In Optical Remote Sensing of the Atmosphere. Optica Publishing Group, 1997. http://dx.doi.org/10.1364/orsa.1997.otub.4.

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The intensity and polarization of skylight, measured at the surface, can be used as a passive remote sensing tool to provide information on the optical properties of aerosols in the atmosphere. Wang and Gordon1 have discussed techniques to use measurements of the intensity of skylight to obtain much of the aerosol phase function. Zhang and Gordon (this meeting) show that elements of the aerosol polarized scattering matrix (Mueller matrix) can be obtained if the Stokes vector of the downwelling skylight is known.2
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Li, J. "Parameterization of the optical properties of sulfate aerosols." In The 15th international conference on nucleation and atmospheric aerosols. AIP, 2000. http://dx.doi.org/10.1063/1.1361939.

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Gu, Xingfa, Tao Yu, Tianhai Cheng, Guo Jing, Hao Chen, and Donghai Xie. "Latest decade's spatial-temporal properties of aerosols over China." In SPIE Optical Engineering + Applications, edited by James J. Butler, Xiaoxiong Xiong, and Xingfa Gu. SPIE, 2011. http://dx.doi.org/10.1117/12.895300.

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Thrush, E., D. M. Brown, N. Salciccioli, et al. "Optical properties and cross-sections of biological aerosols." In SPIE Defense, Security, and Sensing, edited by Augustus W. Fountain III and Patrick J. Gardner. SPIE, 2010. http://dx.doi.org/10.1117/12.850464.

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10

Cutten, D. R., E. W. McCaul, J. D. Spinhirne, et al. "Comparison of Remotely Measured Multispectral Scattering Parameters For Tropospheric Aerosols." In Optical Remote Sensing of the Atmosphere. Optica Publishing Group, 1993. http://dx.doi.org/10.1364/orsa.1993.the.18.

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Resumen
In Fall 1989 and Spring 1990 the National Aeronautics and Space Administration (NASA) conducted a number of survey flights on the NASA DC-8 aircraft over the Pacific Basin as part of the GLObal Backscatter Experiment (GLOBE). The main objective of these flights was to collect data on tropospheric aerosol backscatter, either by direct measurement or modeled from measurements of selected aerosol microphysical properties that cover a wide range of spatial and temporal scales. The primary intent of collecting these data is to predict the performance of space-borne lidar systems such as the Laser A
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Informes sobre el tema "Aerosols – Optical properties"

1

Borghese, F., P. Denti, and R. Saija. The Optical Properties of Aerosols. Defense Technical Information Center, 1990. http://dx.doi.org/10.21236/ada225007.

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2

Paulson, S. E. Optical Properties of Mixed Black Carbon, Inorganic and Secondary Organic Aerosols. Office of Scientific and Technical Information (OSTI), 2012. http://dx.doi.org/10.2172/1041261.

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3

Sokolik, Irina N. Modeling the Time-Dependent Optical Properties of the Multicomponent Aerosols in the Marine Boundary Layer. Defense Technical Information Center, 2001. http://dx.doi.org/10.21236/ada625610.

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4

Davidovits, Paul. Laboratory Studies of Cloud Particle Formation, Mixing State, and Physiochemical and Optical Properties of Carbonaceous Aerosols. Office of Scientific and Technical Information (OSTI), 2019. http://dx.doi.org/10.2172/1529101.

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5

Meskhidze, Nicholas. Production Mechanism, Number Concentration, Size Distribution, Chemical Composition, and Optical Properties of Sea Spray Aerosols Workshop, Summer 2012. Office of Scientific and Technical Information (OSTI), 2013. http://dx.doi.org/10.2172/1096933.

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6

Rosen, James M. Aerosol Optical Properties of the Free Troposphere. Defense Technical Information Center, 1992. http://dx.doi.org/10.21236/ada265795.

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7

Cappa, Christopher D., and Dean B. Atkinson. Characterizing and Understanding Aerosol Optical Properties: CARES - Final Report. Office of Scientific and Technical Information (OSTI), 2017. http://dx.doi.org/10.2172/1413654.

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Rosen, James M. Traineeship Augmentation for Aerosol Optical Properties Study (FY91 EPSCOR). Defense Technical Information Center, 1995. http://dx.doi.org/10.21236/ada299706.

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Ogren, John A., Patrick S. Sheridan, and Elisabeth Andrews. Cloud-Driven Changes in Aerosol Optical Properties - Final Technical Report. Office of Scientific and Technical Information (OSTI), 2007. http://dx.doi.org/10.2172/917185.

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10

Flynn, Connor, Annette Koontz, Brian Ermold, and Duli Chand. ARM Aerosol Optical Properties (AOP) and its Value-Added Product. Office of Scientific and Technical Information (OSTI), 2018. http://dx.doi.org/10.2172/1433185.

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