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Статті в журналах з теми "Atmospheric dust transport"
Schepanski, Kerstin, Marc Mallet, Bernd Heinold, and Max Ulrich. "North African dust transport toward the western Mediterranean basin: atmospheric controls on dust source activation and transport pathways during June–July 2013." Atmospheric Chemistry and Physics 16, no. 22 (November 15, 2016): 14147–68. http://dx.doi.org/10.5194/acp-16-14147-2016.
Повний текст джерелаToth III, Joseph R., Siddharth Rajupet, Henry Squire, Blaire Volbers, Jùn Zhou, Li Xie, R. Mohan Sankaran, and Daniel J. Lacks. "Electrostatic forces alter particle size distributions in atmospheric dust." Atmospheric Chemistry and Physics 20, no. 5 (March 17, 2020): 3181–90. http://dx.doi.org/10.5194/acp-20-3181-2020.
Повний текст джерелаHeavens, Nicholas G., David M. Kass, James H. Shirley, Sylvain Piqueux, and Bruce A. Cantor. "An Observational Overview of Dusty Deep Convection in Martian Dust Storms." Journal of the Atmospheric Sciences 76, no. 11 (October 16, 2019): 3299–326. http://dx.doi.org/10.1175/jas-d-19-0042.1.
Повний текст джерелаBanks, Jamie R., Anja Hünerbein, Bernd Heinold, Helen E. Brindley, Hartwig Deneke, and Kerstin Schepanski. "The sensitivity of the colour of dust in MSG-SEVIRI Desert Dust infrared composite imagery to surface and atmospheric conditions." Atmospheric Chemistry and Physics 19, no. 10 (May 23, 2019): 6893–911. http://dx.doi.org/10.5194/acp-19-6893-2019.
Повний текст джерелаTakahashi, Y., M. Higashi, T. Furukawa, and S. Mitsunobu. "Change of iron species and iron solubility in Asian dust during the long-range transport from western China to Japan." Atmospheric Chemistry and Physics Discussions 11, no. 7 (July 8, 2011): 19545–80. http://dx.doi.org/10.5194/acpd-11-19545-2011.
Повний текст джерелаGrogan, Dustin F. P., and Terrence R. Nathan. "Passive versus Active Transport of Saharan Dust Aerosols by African Easterly Waves." Atmosphere 12, no. 11 (November 16, 2021): 1509. http://dx.doi.org/10.3390/atmos12111509.
Повний текст джерелаLiu, Z., D. Liu, J. Huang, M. Vaughan, I. Uno, N. Sugimoto, C. Kittaka, et al. "Airborne dust distributions over the Tibetan Plateau and surrounding areas derived from the first year of CALIPSO lidar observations." Atmospheric Chemistry and Physics 8, no. 16 (August 29, 2008): 5045–60. http://dx.doi.org/10.5194/acp-8-5045-2008.
Повний текст джерелаSchepanski, Kerstin, Bernd Heinold, and Ina Tegen. "Harmattan, Saharan heat low, and West African monsoon circulation: modulations on the Saharan dust outflow towards the North Atlantic." Atmospheric Chemistry and Physics 17, no. 17 (September 1, 2017): 10223–43. http://dx.doi.org/10.5194/acp-17-10223-2017.
Повний текст джерелаOsada, K., S. Ura, M. Kagawa, M. Mikami, T. Y. Tanaka, S. Matoba, K. Aoki, et al. "Wet and dry deposition of mineral dust particles in Japan: factors related to temporal variation and spatial distribution." Atmospheric Chemistry and Physics 14, no. 2 (January 29, 2014): 1107–21. http://dx.doi.org/10.5194/acp-14-1107-2014.
Повний текст джерелаVoss, Kara K., Amato T. Evan, Kimbery A. Prather, and F. Martin Ralph. "Dusty Atmospheric Rivers: Characteristics and Origins." Journal of Climate 33, no. 22 (November 15, 2020): 9749–62. http://dx.doi.org/10.1175/jcli-d-20-0059.1.
Повний текст джерелаДисертації з теми "Atmospheric dust transport"
Mulholland, David Paul. "Martian dust lifting, transport and associated processes." Thesis, University of Oxford, 2012. http://ora.ox.ac.uk/objects/uuid:a94d810a-5c55-4b7e-84b4-04d4f3b4f191.
Повний текст джерелаEngelstaedter, Sebastian. "An analysis of the role of the atmosphere in modulating desert dust variability : controls on emission and atmospheric transport." Thesis, University of Oxford, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.443725.
Повний текст джерелаWei, Chao. "Modeling the effects of heterogeneous reactions on atmospheric chemistry and aerosol properties." Diss., University of Iowa, 2010. https://ir.uiowa.edu/etd/903.
Повний текст джерелаNewton, Seth. "Occurrence and fate of emerging and legacy flame retardants : from indoor environments to remote areas." Doctoral thesis, Stockholms universitet, Institutionen för miljövetenskap och analytisk kemi, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-116443.
Повний текст джерелаAt the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 3: Manuscript. Paper 4: Manuscript.
Silva, Marcio Cataldo Gomes da. "Características biogeoquímicas da interação atmosfera criosfera na Antártica ocidental." Universidade do Estado do Rio de Janeiro, 2011. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=3339.
Повний текст джерелаO manto polar antártico retêm informação paleoclimatologica por entres suas camadas de neve e gelo. O gelo antártico tem revelado a base de dados paleoclimática de maior resolução para os últimos 800 mil anos. Os padrões de transporte atmosférico refletem a composição e a fonte do particulado encontrado na neve e no gelo do continente Antártico. Estando relacionado a processos climáticos, as características desse transporte alteram em quantidade e qualidade as espécies químicas que se depositam sobre o manto de gelo. Dessa forma, o estudo dos depósitos de particulado ao longo das camadas de neve/gelo na Antártica pode sugerir mudanças nos padrões de transporte atmosférico. Atualmente a comunidade científica discute as diferenças de padrões climáticos entre o leste e o oeste antártico. Enquanto de forma geral observa-se instabilidade no setor oeste, o clima da antártica oriental demonstra relativa estabilidade climática. Neste estudo, analisamos dois testemunhos de gelo recente de duas regiões com características climáticas diferentes do continente Antártico. No Platô Detroit situado na Península Antártica (6410′S/0600′O), analisamos a variabilidade de Black Carbon (BC) ao longo de 20 metros de neve. O BC encontrado na Península Antártica apresentou baixas concentrações comparáveis as encontradas no gelo do Artico período pré-industrial. Nossos resultados sugerem que sua variabiliade corresponde à sazonalidade dos períodos de queimada nos continentes do Hemisfério Sul. No interior do continente Antártico, analisamos o particulado em geral por um processo de microanálise ao longo de um testemunho de 40 metros extraído em Mont Johns (79o55′S/09423′O). Encontramos uma tendência negativa na deposição de poeira mineral (AlSi) entre 1967 e 2007. Nossos resultados sugerem que esta tendência seja resultado de um crescente isolamento atmosférico da região central do continente antártico pelo aumento da intensidade dos ventos ao redor da Antártica. Este aumento na intensidade dos ventos reflete por sua vez o resfriamento da alta atmosfera no centro antártico causado pela depleção da camada de ozônio na região. Adicionalmente, amostras de diferentes microambientes de Patriot Hills (8018′S/08121′O) foram coletadas de maneira asséptica para análise microbiológica. As amostras foram cultivadas em meio R2 e paralelamente o DNA total extraído foi sequenciado pela técnica de pirosequenciamento. Os resultados preliminares desta analise mostram grande riqueza de espécies dos mais variados grupos. Os resultados deste trabalho caracterizam três diferentes parâmetros relacionados a deposição atmosférica em duas áreas pouco exploradas e de grande interesse científico do continente antártico.
The antarctic ice cap stores paleoclimatological information within layers of snow and ice. Antarctic ice has revealed the higher resolution paleoclimactic database for the last 800 kyr. Atmospheric transport plays a fundamental role on the composition and sources of particulate matter found in the Antarctic ice. It has been related to several climatic processes that changes the quantity and quality of exogenous aerosols reaching Antarctica. Therefore, studies of the particulate matter deposits along the snow/ice layers may suggest changes on atmospheric transport patterns. This work, analyze two recent ice cores from two climatic distinct regions of the Antarctic continent. One retrieved from Detroit Plateau/Antarctic Peninsula (6410′S/0600′W), in which we have analyze Black Carbon (BC) deposition and variability along 20 meters of snow. BC found in the Antarctic Peninsula showed low concentrations (varing between 0,014 and 3,733ppb), comparable to the concentrations found on Arctic ice dated from before the industrial revolution period. Our results suggest that peaks of BC detected correspond, mostly, to biomass burning seasons in the South Hemisphere, not speficically from South America. The second one, of 40 m, was retrieved from Central-West Antarctica, Mont Johns (79o55′S/094 23′W), in which we analyzed the mineral dust abundance thought M.E.V. E.D.X. technique. In this study we found negative trends in mineral dust (inferred from Fe, Ti and AlSi) deposition between 1967 and 2007, in contrast to similar works in Sub-antarctic regions. We demonstrate that this trend is a consequence of the persistent atmospheric isolation that encloses the Central and East Antarctic regions due to the increasing winds around Antarctica within this period. It has been documented that westerlies intensification reflect the upper atmosphere cooling above Central Antarctica caused by the stratospherical ozone layer depletion. As part of the polar site characterization, we additionally have performed sampling for microbiological purpose from distinct microenvironments at Patriot Hills (8018′S/08121′W). Samples were cultivated on R2 media and at the same time total DNA on samples was extracted and sent to a pyrosequencing analysis. Preliminary results show richness and diversity of bacterial species distributed on five phyla.
Qu, Zihan. "Chemical properties of continental aerosol transported over the Southern Ocean : Patagonian and Namibian sources." Thesis, Paris 6, 2016. http://www.theses.fr/2016PA066002/document.
Повний текст джерелаMineral dust is considered to be an important supplier of micronutrient for the Southern Ocean where the primary production is limited by insufficient supply of micronutrients. Patagonia (South America) and Namibia (Southern Africa) are two main dust sources for the South Atlantic section of the Southern Ocean. Emission inventories of bioavailable micronutrients from these two regions regulate the final biological impact on marine ecosystem in the South Atlantic Ocean. This thesis is mainly focused on the investigation of 1) the atmospheric dust concentration and its temporal pattern in Patagonia, 2) the spatial heterogeneity of dust elemental composition in Patagonia and Namibia, and 3) the pH dependence of elemental solubility in Patagonian and Namibian dust. These three aspects are the key issues to model the emission inventories of bioavailable micronutrients from dust sources. Dust concentration measurements were conducted in Patagonia-Atlantic Coast and revealed a seasonal pattern of dust concentration with lower dust level in winter than the other three seasons. Meteorological records suggest that this seasonal pattern is associated with the variation of soil moisture in source areas rather than the recurrently high wind speed. Dust samples were generated from Patagonian and Namibian soils to investigate the elemental composition and the elemental solubility of source dust. Dust elemental composition differs to different degrees from their parents soils, particularly in Namibia due to the dilution effect of quartz in soil. Spatial variability of dust elemental composition was observed at both continental scale and regional scale in Patagonia and Namibia. Variations in Ca and Mg content are the main reasons for the spatial heterogeneity of dust elemental composition. Elemental solubility of Patagonian and Namibian dust increased with acidity of leaching solution. More soluble elements namely Ca, K, Mg, Mn, Sr and Ba showed much higher solubility in calcium-rich dust due to the presence of carbonate. The dust concentration record obtained in Patagonia may help to better quantify the dust emission in subantarctic region and to constrain dust models. Database of dust elemental composition and elemental solubility in Patagonia and Namibia also contributes to the evaluation of emission inventories of soluble elements from dust sources to the Southern Ocean
Haga, Donna. "Ice nucleation by mineral dusts, fungal spores, and bacteria : implications for climate and the long-distance transport of these aerosols in the atmosphere." Thesis, University of British Columbia, 2013. http://hdl.handle.net/2429/45241.
Повний текст джерелаHuei, Chang Ming, and 張銘惠. "Atmospheric Particulate PAH Patterns of China Long-Range Transport Dust Storms and Taiwan Local Festival Celebration Events." Thesis, 2009. http://ndltd.ncl.edu.tw/handle/b7hgvu.
Повний текст джерела輔仁大學
公共衛生學系碩士班
97
PAHs, by products of incomplete combustion or pyrolysis of hydrocarbons, can be regarded as important representative chemicals on long-range transportation particles. Moreover, the concentrations and patterns of particle-bound PAHs in the atmosphere are used as indicators of regional air quality to assess the exposure risk to human health. In recent years, many PAHs sources, such as vehicle exhaust, stack gas etc. have contributed to the PAHs levels in the Taiwan atmosphere. In addition to local sources, the notable events include dust storm particles from China, firework and barbecue smoke in Taiwan local festival events. This study discussed the characteristic ratios (CR) of PAHs and distinguished possible PAHs sources in various scenarios. This study collected airborne PAHs samples on the Fu Jen University campus from 2007 to 2008. A Micro-Orifice Uniform Deposit Impactor (MOUDI ) instrument was used to collected particle size segregated samples in the dust storm events in 2002-2008. This study also used filters and gas adsorbent (F/A) samplers to collect particulate matters and gaseous PAHs in Ghost Festival and Moon Festival in 2007-2008. The final portion of this study was to examine the pollution extent of smoke particles in the firework event at Tainan Yanshuai in 2009. The 34 PAHs results showed that air samples taken from different heights (altitude of 10 meters and 20 meters from the sea level) showed no statistically significant difference with respect to particulate mass concentration and 34 PAH concentrations. These results were pooled and regarded as the PAHs background level in Taipei. Similar PAHs patterns were found in Tainan background with lower concentrations. The major gas-phase PAHs included Naph, 2mN, 1mN and BP, whereas the main solid-phase PAHs were BbF, BghiP, IcdP. The average atmospheric particle-PAHs concentration in 2007 Ghost Festival was 9.08 ng/m3, which was much higher than the background level (2.35 ± 1.99 ng/m3). One possible explanation is that significant amounts of resemble money for the dead was burned during the Ghost festival. Mass concentrations of total suspended particulate (TSP) in the Tainan Yanshuai firework are 265.1 ~ 844.8 μg/m3, far above the EPA air quality standards (250 μg/m3). Additionally, fireworks used during the Yanshuai festival caused atmospheric PAHs concentrations rising to 42.0 ~ 71.1 ng/m3 which was 10 times higher than the background condition. At the same time, the concentration of BaP in the firework event also increased significantly, 0.06~0.46 ng/m3, implying the potential health hazards. By using the characteristic ratios (CR) related to BbF, this study also found that the dust storm events attributed significant particle-bound PAHs to Taiwan. The CRs of BkF and BaP were found to be significantly higher than the background CRs as dust particles were transported through North China, originally from Mongolia. At the mixing layer below 1000 m, the dust storm particles are likely mixed with regional airborne pollutants, such as PAHs, then migrated to the down wind locations. This study suggested that the comparison of particle-bound PAH CRs along the NOAA backward trajectory routes to Taiwan could provide more information in describing PAH partitioning phenomena during the dust particle transportation. The significant contribution of TSP mass and PAHs concentrations are followed by the orders of Yanshuai fireworks, dust storm, Ghost Festival and Moon Festival. The applications of PAH CR values can be used to distinguished particle-bound origins from the local pollution sources in the dust storm long range transportion. However, more regional PAHs patterns in the dust storm pathways were needed to evaluate the possible aerosol-pollutant interaction mechanism during the transportation.
Santee, Michelle. "The thermal structure, dust loading, and meridional transport in the Martian atmosphere during late southern summer." Thesis, 1993. https://thesis.library.caltech.edu/7384/1/Santee_m_1993.pdf.
Повний текст джерелаThis thesis consists of two papers, both of which investigate the state of the Martian atmosphere during a relatively clear period in late southern summer. The first paper describes a new technique for the simultaneous retrieval of atmospheric temperatures and dust abundances from thermal emission spectra. The second paper describes a diagnostic stream function model which is used with the temperature and dust results of the first paper to solve for the meridional and vertical components of the diabatic circulation simultaneously. The abstracts for the two papers are reproduced below.
PAPER I:
The temperature structure and dust loading of the Martian atmosphere are investigated using thermal emission spectra recorded by the Mariner 9 infrared interferometer spectrometer (IRIS). The analysis is restricted to a subset of the IRIS data consisting of approximately 2400 spectra in a 12-day period extending from L_s = 343° to L_s = 348°, corresponding to late southern summer on Mars. Simultaneous retrieval of the vertical distribution of both atmospheric temperature and dust optical depth is accomplished through an iterative procedure which is performed on each spectrum. The inclusion of dust opacity in the retrieval algorithm causes the retrieved temperatures to change by more than 20 K in some atmospheric layers. The largest column-integrated 9 µm dust optical depths (~ 0.4) occur over the equatorial regions. The highest atmospheric temperatures (> 260 K) are found at low altitudes near the sub-solar latitude (~ 6° s), while the coldest temperatures (˂ 150 K) are found at levels near 1.0 mbar over the winter pole. A comparison of temperature maps for 2 PM and 2 AM indicates diurnal temperature variations as large as 80 K at low altitudes near the sub- solar latitude, whereas diurnal temperature changes at pressures less than 1.0 mbar are typically about 10 K. Both dayside and nightside temperatures above about 0.1 mbar (~ 40 km) are warmer over the winter (north) polar region than over the equator or the summer (south) polar region. This thermal structure suggests the existence of a net zonally-averaged meridional circulation with rising motion at low latitudes, poleward flow at altitudes above 40 km, and subsidence over the poles. Because a meridional circulation transports atmospheric constituents as well as heat, it has significant implications for the net flux of dust and water into the polar regions.
PAPER II:
The circulation of the Martian atmosphere during late southern summer is calculated diagnostically from the observed atmospheric temperature distribution. We use global maps of temperature and dust optical depth (~ 0-60 km) retrieved from a subset of the Mariner 9 IRIS thermal emission spectra spanning L_s = 343°- 348° [Santee and Crisp, 1992]. This thermal structure is characterized by a reversed meridional temperature gradient (temperatures increasing poleward) at altitudes above about 40 km. Zonal- mean zonal winds are derived from the zonally-averaged temperatures assuming gradient wind balance and zero surface zonal wind. Both hemispheres have intense mid- latitude westerly jets (with velocities of 80- 90 m/s near 50 km); in the southern tropics the winds are strongly easterly (with velocities of 100 m/s near 50 km). The north-south atmospheric transport includes contributions from the zonal- mean meridional circulation and large-scale waves. Their net effect can be approximated by the diabatic circulation, which is that circulation needed to maintain the observed temperature distribution (warm winter pole, cool tropics) in the presence of the radiative forcing. A radiative transfer model [Crisp, 1990] which accounts for absorption, emission and multiple scattering by particles and non- grey gases is used to compute the solar heating and thermal cooling rates from diurnal averages of the retrieved IRlS temperature and dust distributions. At pressures below 4 mbar, there are large net heating rates (up to 8 K/ day) in the equatorial region and large net cooling rates (up to 20 K/ day) in the polar regions. These net heating rates are used in a diagnostic stream function model which solves for the meridional and vertical components of the diabatic circulation simultaneously. We find a two-cell circulation, with upwelling over the equator(~ 1.5 cm/s), poleward motion in both hemispheres(~ 2 m/s), and subsidence over the poles (1-2 cm/ s). This circulation is sufficiently vigorous that the meridional transport time scale is ~ 13 days. Vertical transport is primarily advective in nature, except in the high-altitude winter polar regions, where diffusive processes dominate. Water vapor desorbed from the low-latitude regolith during late northern winter/ early northern spring may be transported upward by the ascending branch of this circulation, where it would be transported poleward by the high-altitude meridional winds. This process could provide a high-altitude source of water vapor for the polar hood.
Книги з теми "Atmospheric dust transport"
1946-, Leinen Margaret, Sarnthein M, and North Atlantic Treaty Organization, eds. Paleoclimatology and paleometeorology: Modern and past patterns of global atmospheric transport. Dordrecht: Kluwer Academic Publishers, 1989.
Знайти повний текст джерелаLeinen, Margaret, and Michael Sarnthein. Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport. Springer, 2012.
Знайти повний текст джерелаLeinen, Margaret, and Michael Sarnthein. Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport. Springer, 2012.
Знайти повний текст джерела(Editor), Margaret Leinen, and Michael Sarnthein (Editor), eds. Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport (NATO Science Series C: (closed)). Springer, 2007.
Знайти повний текст джерелаLau, William K. M. Impacts of Aerosols on Climate and Weather in the Hindu-Kush-Himalayas-Gangetic Region. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.590.
Повний текст джерелаVaughan, David. 4. Earth’s surface and the cycling of minerals. Oxford University Press, 2014. http://dx.doi.org/10.1093/actrade/9780199682843.003.0004.
Повний текст джерелаDagsson-Waldhauserova, Pavla, and Outi Meinander, eds. Atmosphere – Cryosphere Interaction in the Arctic, at High Latitudes and Mountains with Focus on Transport, Deposition and Effects of Dust, Black Carbon, and other Aerosols. Frontiers Media SA, 2020. http://dx.doi.org/10.3389/978-2-88963-504-7.
Повний текст джерелаЧастини книг з теми "Atmospheric dust transport"
Merrill, J., R. Arimoto, G. Bergametti, S. Joussaume, S. Thompson, and D. Westphal. "Dust Transport and Transport Modeling." In Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport, 865–68. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0995-3_37.
Повний текст джерелаTetzlaff, G., M. Peters, W. Janssen, and L. J. Adams. "Aeolian Dust Transport in West Africa." In Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport, 185–203. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0995-3_7.
Повний текст джерелаSchuetz, Lothar. "Atmospheric Mineral Dust - Properties and Source Markers." In Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport, 359–83. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0995-3_15.
Повний текст джерелаNickling, W., A. Brazel, D. Gillette, N. J. Middleton, K. Pye, P. Rognon, and G. Tetzlaff. "Dust Formation, Injection, and Continental Aridity." In Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport, 861–63. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0995-3_36.
Повний текст джерелаBrazel, Anthony J. "Dust and Climate in the American Southwest." In Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport, 65–96. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0995-3_3.
Повний текст джерелаKambezidis, H. D., A. G. Paliatsos, N. Kappos, and B. Kasselouri. "A Case of African Dust Transport over Athens Captured by a Ceilometer." In Advances in Meteorology, Climatology and Atmospheric Physics, 1011–18. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29172-2_141.
Повний текст джерелаBūcher, A. "Fallout of Saharan Dust in the Northwestern Mediterranean Region." In Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport, 565–84. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0995-3_24.
Повний текст джерелаJoussaume, S. "Desert Dust and Climate : An Investigation Using an Atmospheric General Circulation Model." In Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport, 253–63. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0995-3_10.
Повний текст джерелаPye, K. "Processes of Fine Particle Formation, Dust Source Regions, and Climatic Changes." In Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport, 3–30. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0995-3_1.
Повний текст джерелаTetzlaff, G., R. Arimoto, G. Bergametti, G. Coude-Gaussen, G. A. d’Almeida, G. Eglinton, F. Grousset, L. Schütz, F. Sirocko, and L. Tomadin. "Dust Composition and Factors Controlling it: Evidence from Aerosols and Sediments." In Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport, 869–71. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0995-3_38.
Повний текст джерелаТези доповідей конференцій з теми "Atmospheric dust transport"
Kalinskaya, Darya V., and Alla Varenik. "The research of the dust transport impact on the biogeochemical characteristics of the Black Sea surface layer." In XXV International Symposium, Atmospheric and Ocean Optics, Atmospheric Physics, edited by Gennadii G. Matvienko and Oleg A. Romanovskii. SPIE, 2019. http://dx.doi.org/10.1117/12.2540432.
Повний текст джерелаSurmava, Aleksandre, Demuri Demetrasvili, Vepkhia Kukhalashvili, and Natia Gigauri. "NUMERICAL MODELLING OF DUST DISTRIBUTION IN THE ATMOSPHERE OF A CITY WITH COMPLEX RELIEF." In GEOLINKS International Conference. SAIMA Consult Ltd, 2020. http://dx.doi.org/10.32008/geolinks2020/b1/v2/04.
Повний текст джерелаTong, Xiaoling. "Numerical Modeling of Dust Transport Around Moving Vehicles in Unsteady Atmospheric Boundary Layer Using Precursor Simulation." In AIAA Scitech 2021 Forum. Reston, Virginia: American Institute of Aeronautics and Astronautics, 2021. http://dx.doi.org/10.2514/6.2021-1541.
Повний текст джерелаCharles, Leona, Barry Gross, Yonghua Wu, Viviana Vladutescu, Fred Moshary, and Sam Ahmed. "Atmospheric transport of smoke and dust particulates and their interaction with the Planetary Boundary Layer as observed by multi-wavelength lidar and supporting instrumentation." In Optical Engineering + Applications, edited by Upendra N. Singh. SPIE, 2007. http://dx.doi.org/10.1117/12.731943.
Повний текст джерелаGelain, Thomas, Laurent Ricciardi, and François Gensdarmes. "Implementation of a Particle Resuspension Model in a CFD Code: Application to an Air Ingress Scenario in a Vacuum Toroidal Vessel." In 2020 International Conference on Nuclear Engineering collocated with the ASME 2020 Power Conference. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/icone2020-16139.
Повний текст джерелаHumphries, Larry, Brad Beeny, David Louie, Hossein Esmaili, and Michael Salay. "Non-LWR Model Development for the MELCOR Code." In 2018 26th International Conference on Nuclear Engineering. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/icone26-82415.
Повний текст джерелаJena, Sofen K., and Swarup K. Mahapatra. "Effect of Participating Medium Radiation and Nano-Fluidic Behaviour of Atmospheric Aerosol on Natural Convection of Industrial Dusty Air." In ASME 2013 4th International Conference on Micro/Nanoscale Heat and Mass Transfer. American Society of Mechanical Engineers, 2013. http://dx.doi.org/10.1115/mnhmt2013-22259.
Повний текст джерелаMazumder, M. K., R. Sharma, A. S. Biris, S. Trigwell, M. N. Horenstein, and M. M. Abbas. "Electrostatic and Gravitational Transport of Lunar Dust in the Airless Atmosphere of the Moon." In 2008 IEEE Industry Applications Society Annual Meeting (IAS). IEEE, 2008. http://dx.doi.org/10.1109/08ias.2008.124.
Повний текст джерелаEllis, Hershle, Chase Casher, Jamal Longwood, Abel Taye, Laura Ruhala, and Richard Ruhala. "Lunar Cargo Transportation (LuCaT): Semi-Autonomous Vehicle With Suspended Cable and Solar Power." In ASME 2020 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/imece2020-24197.
Повний текст джерелаParozzi, F., and S. Paci. "Development and Validation of the ECART Code for the Safety Analysis of Nuclear Installations." In 14th International Conference on Nuclear Engineering. ASMEDC, 2006. http://dx.doi.org/10.1115/icone14-89275.
Повний текст джерелаЗвіти організацій з теми "Atmospheric dust transport"
Gallagher, Alex, Sandra LeGrand, Taylor Hodgdon, and Theodore Letcher. Simulating environmental conditions for Southwest United States convective dust storms using the Weather Research and Forecasting Model v4.1. Engineer Research and Development Center (U.S.), August 2022. http://dx.doi.org/10.21079/11681/44963.
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