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References

  • Adams, J. W., D. Rodriguez, and R. A. Cox (2005), The uptake of SO2 on Saharan dust: A flow tube study, Atmos. Chem. Phys., 5, 26792689.
  • Alpert, P., and G. Ganor (1993), A jet stream associated heavy dust storms in the western Mediterranean, J. Geophys. Res., 98, 73397349.
  • Anderberg, M. R. (1973), Cluster analysis for applications, Academic Press, New York.
  • Banacos, P. C., and M. L. Ekster (2010), The association of the elevated mixed layer with significant severe weather events in the Northeast United States, Weather Forecasting, 25, 10821102.
  • Barkan, J., and P. Alpert (2010), Synoptic analysis of a rare event of Saharan dust reaching the Arctic region, Weather, 65, 208211.
  • Barkan, J., H. Kutiel, and P. Alpert (2004), Climatology of dust sources in North Africa and the Arabian Peninsula, based on TOMS data, Indoor Built Environ., 13, 407419.
  • Barnes, W. L., T. S. Pagano, V. V. Salomonson, E. S. Directorate, N. Center, and M. D. Greenbelt (1998), Prelaunch characteristics of the moderate resolution imaging spectroradiometer (MODIS) on EOS-AM1, IEEE T. Geosci. Remote, 36, 10881100.
  • Brimelow, J. C., and G. W. Reuter (2005), Transport of atmospheric moisture during three extreme rainfall events over the Mackenzie River Basin, J. Hydrometeorology, 6, 423440.
  • Bryson, R. A., and D. A. Barreis (1967), Possibilities of major climatic modifications and their implications: Northwest India, a case for study, Bull. Am. Meteorol. Soc., 48, 136142.
  • Cabello, M., et al. (2012), Spatial and temporal variation of the impact of an extreme Saharan dust event, J. Geophys. Res., 117, D11204, doi:10.1029/2012JD017513.
  • Chen, Y. S., P. C. Sheen, E. R. Chen, Y. K. Liu, T. N. Wu, and C. Y. Yang (2004), Effects of Asian dust storm events on daily mortality in Taipeh, Taiwan, Environ. Res., 95, 151155.
  • Clements, T., R. O. Stone, J. F. Mann, and J. L. Eymann (1963), A study of windborne sand and dust in desert areas. Technical Report ES-8. US Army Natick Laboratories, Earth Science Division, Natick, Mass.
  • Čolović-Daul (2007), Lidar sensing of aerosols and determination of their trajectories, Master's thesis, University of Nova Gorica, 77 pp.
  • Conte, M., M. Colarino, and E. Piervitali (1996), Atlantic disturbances deeply penetrating the African continent: Effect over Saharan regions and the Mediterranean basin, in The Impact of Desert Dust Across the Mediterranean., pp. 93102, Kluver Acad.: Norwell Mass.
  • Crawford, J., W. Zahorowski, and D. D. Cohen (2009), A new metric space incorporating radon-222 for generation of back trajectory clusters in atmospheric pollution studies, Atmos. Environ., 43, 371381.
  • Dayan, U., J. Hefter, J. Miller, and G. Gutman (1991), Dust intrusion events into the Mediterranean basin, J. Appl. Meteor., 30, 11881193.
  • Delany, A. C., D. W. Parkin, E. D. Goldberg, B. E. F. Riemann, and J. J. Griffin (1967), Airborne dust collected at Barbados, Geochim. Cosmochim. Acta, 31, 895909.
  • Dong, C., Y. Liu, M. Lankhorst, D. Chen, J. C. McWilliams, and Y. Guan (2011), A scheme to identify loops from trajectories of oceanic surface drifters: An application in the Kuroshio Extension region, J. Atmos. Oceanic Technol., 28, 11671176.
  • Dorling, S. R., T. D. Davies, and C. E. Pierce (1992), Cluster analysis: A technique for estimating the synoptic meteorological controls on air and precipitation chemistry – method and applications, Atmos. Environ., 26, 25752581.
  • Draxler, R. R. (2006), US National Oceanic and Atmospheric Administration (NOAA), HYbrid Single- Particle Lagrangian Integrated Trajectory Model, http://www.arl.noaa.gov/ready/hysp_info.html.
  • Draxler, R. R., and G. D. Hess (1998), An overview of the HYSPLIT-4 modelling system for trajectories, dispersion and deposition. Aust. Meteorol. Mag., 47, 295308.
  • Draxler, R. R., and G. D. Rolph (2012), HYSPLIT (HYbrid Single-Particle Lagrangian Integrated Trajectory) model access via NOAA ARL READY Website (http://www.arl.noaa.gov/ready/hysplit4html), NOAA Air Resourc. Lab., Silver Spring, Md.
  • Dunion, J. P., and C. S. Velden (2004), The impact of the Saharan air layer on Atlantic tropical cyclone activity, Bull. Amer. Meteor. Soc., 84, 353365.
  • Dutton, J. A. (1986), The Ceaseless Wind: An Introduction to the Theory of Atmospheric Motion, Dover, New York.
  • Escudero, M., et al. (2005), Wet and dry African dust episodes over eastern Spain, J. Geophys. Res., 110, D18D08, doi:10.1029/2004JD004731.
  • Escudero, M., A. F. Stein, R. R. Draxler, X. Querol, A. Alastuey, S. Castillo, and A. Avilla (2011), Source apportionment for African dust outbreaks over the Western Mediterranean using the HYSPLIT model, Atmos. Res., 99, 518527, doi:10.1016/j.atmosres.2010.12.002.
  • Estellés, V., J. A. Martinez-Lozano, and M. A. P. Utrillas (2007), Influence of air mass history on the columnar aerosol properties at Valencia, Spain, J. Geophys. Res., 112, D15211, doi:10.1029/2007JD008593.
  • Everitt, B. (1980), Cluster Analysis, Halstead, 136 pp.
  • Fryrear, D. W. (1981), Long-term effect of erosion and cropping on soil productivity, Geol. Soc. Am., 186, 253259.
  • Ganor, E., and Y. Mamane (1982), Transport of Saharan dust across the eastern Mediterranean, Atmos. Environ., 16, 581587.
  • Ganor, E., H. A. Foner, S. Brenner, E. Neeman, and N Lavi (1991), The chemical composition of aerosols settling in Israel following dust storms, Atmos. Environ., 25, 26652670.
  • Gatz, D. F., and J. M. Prospero (1996), A large silicon-aluminum aerosol plume in central Illinois: North African desert dust?, Atmos. Environ., 30, 37893799.
  • Giles, J. (2005), The dustiest place on Earth, Nature, 434, 816819.
  • Ginoux, P. A., J. M. Prospero, T. E. Gill, C. Hsu, and M. Zhao (2012), Global-scale attribution of anthropogenic and natural dust sources and their emission rates based on MODIS Deep Blue aerosol products, Review of Geophysics, 50, RG3005, doi:10.1029/2012RG000388.
  • Goudie, A. S., and N. J. Middleton (2001), Saharan dust storms: nature and consequences, Earth- Science Reviews, 56, 179204.
  • Goudie, A. S., and N. J. Middleton (2006), Desert Dust in the Global System, Heidelberg, Springer.
  • Gruber, N., and J. L. Sarmiento (1997), Global patterns of marine nitrogen fixation and denitrification, Global Biogeochem. Cycles, 11, 235266.
  • Gyan, K., et al. (2005), African dust clouds are associated with increased paediatric asthma accident and emergency admissions on the Caribbean island of Trinidad, Int. J. Biometeorol., 49, 371376.
  • Hagen, L. J., and N. P. Woodruff (1973), Air pollution from dust storms in the Great Plains, Atmos. Environ., 7, 323332.
  • Hansen, J., M. Sato, A. Lacis, R. Ruedy, I. Tegen, and E. Matthews (1998), Climate forcing in the industrial era, Proc. Natl. Acad. Sci. U. S. A., 95, 1275312758, doi:10.1073/pnas.95.22.12753.
  • Haywood, J., and O. Boucher (2000), Estimates of the direct and indirect radiative forcing due to tropospheric aerosols: A review, Rev. Geophys., 38, 513543, doi:10.1029/1999RG000078.
  • Haywood, J., et al. (2003), Radiative properties and direct radiative effect of Saharan dust measured by the C-130 aircraft during SHADE: 1. Solar spectrum, Journal of Geophysical Research, 108, D188577, doi:10.1029/D2002JD002687.
  • Herut, B., and M. Krom (1996), Atmospheric input of nutrients and dust to the SE Mediterranean. In: The Impact of Desert Dust Across the Mediterranean, S Guerzoni, R Chester (eds), pp. 349358, Kluwer, Dordrecht.
  • Hsu, N. C., S. -C. Tsay, M. King, and J. R. Herman (2004), Aerosol properties over bright-reflecting source regions, IEEE Trans. Geosci. Remote Sens., 42, 557569.
  • Hsu, N. C., S. -C. Tsay, M. King, and J. R. Herman (2006), Deep Blue retrievals of Asian aerosol properties during ACE-Asia, IEEE Trans. Geosci. Remote Sens., 44, 31803195.
  • Jickells, T. D., S. Dorling, W. G. Deuser, T. M. Church, R. Arimoto, and J. M. Prospero (1998), Air-borne dust fluxes to a deep water sediment trap in the Sargasso Sea, Global Biogeochem. Cycles, 12, 311320.
  • Jorba, O., C. Pérez, F. Rocadenbosch, and J. M. Baldasano (1997 to 2002), Cluster analysis of 4-day back trajectories arriving in the Barcelona area, Spain, J. Appl. Meteorol., 43, 887901.
  • Junge, C. (1979), The importance of mineral dust as an atmospheric constituent, in Saharan Dust, Scope 14, C. Morales (ed), pp. 4960, John Wiley & Sons, New York.
  • Kalnay, E., et al. (1996), The NCEP/NCAR 40-year reanalysis project, Bull. Am. Meteorol. Soc., 77, 437471.
  • Kampa, M., and E. Castanas (2008), Human health effects of air pollution, Environ. Pollut., 151, 362367, doi:10.1016/j.envpol.2007.06.012.
  • Kanamitsu, M. 1989, Description of the NMC global data assimilation and forecast system, Wea. Forecasting, 4, 335342.
  • Kar, A., and K. Takeuchi (2004), Yellow dust: An overview of research and felt needs, J. Arid Environ., 59, 167187.
  • Karyampudi, V. M., and T. N. Carlson (1988), Analysis and numerical simulations of the Saharan air layer and its effect on easterly wave disturbances, J. Atmos. Sci., 45, 31023136.
  • Karyampudi, V. M., and H. F. Pierce (2002), Synoptic-scale influence of the Saharan air layer on tropical cyclogenesis over the eastern Atlantic, Mon. Wea. Rev., 130, 31003128.
  • Kaufman, L., and P. J. Rousseeuw (1989), Finding Groups in Data: An Introduction to Cluster Analysis, Wiley Series in Probability and Mathematical Statistics, John Wiley & Sons, Hoboken, NJ.
  • Kaufman, L., and P. J. Rousseeuw (2008), Finding Groups in Data: An Introduction to Cluster Analysis, John Wiley & Sons, Hoboken, NJ, 342 pp.
  • Kubilay, N., S. Nickovic, C. Moulin, and F. Dulac (2000), An illustration of the transport and deposition of mineral dust onto the eastern Mediterranean, Atmos. Environ., 34, 12931303.
  • Kubilay, N., T. Cokacar, and T. Oguz (2003), Optical properties of mineral dust outbreaks over the northeastern Mediterranean, J. Geophys. Res., 108, D21, doi:10.1029/2003JD003798.
  • Kubilay, N., T. Oguz, M. Kocak, and O. Torres (2005), Ground-based assessment of total ozone mapping spectrometer (TOMS) data for dust transport over the northeastern Mediterranean, Global Biogeochem. Cycles, 19, GB1022, doi:10.1029/2004GB002370.
  • Koch, J., and N. O. Renno (2005), The role of convective plumes and vortices on the global aerosol budget, Geophys. Res. Lett., 32, L18806, doi:10.1029/2005GL023420.
  • Kutiel, H., and J. Furman (2003), Dust storms in the Middle East: Sources of origin and their temporal characteristics, Indoor Built Environ., 12, 419426.
  • Lau, K. M., and J. M. Kim (2007a), How nature foiled the 2006 hurricane forecasts, Eos. Trans. Amer. Geophys. Union, 88, doi:10.1029/2007E0090002.
  • Lau, K. M., and J. M. Kim (2007b), Cooling of the Atlantic by Saharan dust, Geophys. Res. Lett., 34, L23811, doi:10.1029/2007GL031538.
  • Leathers, C. R. (1981), Plant components of desert dust in Arizona and their significance for man. In: Péwé TL (ed) Desert dust. Geol Soc Am Spec Pap, 186, 191206.
  • Lee, Y. C., X. Yang, and M. Wenig (2010), Transport of dusts from East Asian and non-East Asian sources to Hong Kong during dust storm related events 1996–2007, Atmos. Environ., 44, 37283738.
  • Lin, C. L., M. D. Cheng, and W. H. Schroeder (2001), Transport patterns and potential sources of total gaseous mercury measured in Canadian high Arctic in 1995, Atmos. Environ., 35, 11411154.
  • Logan, T., B. Xi, X. Dong, R. Obrecht, Z. Li, and M. Cribb (2010), A study of Asian dust plumes using satellite, surface, and aircraft measurements during the INTEX-B field experiment, J. Geophys. Res., 115, D00K25, doi:10.1029/2010JD014134.
  • Lohmann, U., and J. Feichter (2005), Global indirect aerosol effects: A review, Atmos. Chem. Phys., 5, 715737, doi:10.5194/acp-5-715-2005.
  • Maley, J. (1982), Dust, clouds, rain types and climatic variations in tropical north Atlantic, Quat. Res., 18, 16.
  • Marey, H. S., J. C. Gille, H. M. El-Askary, E. A. Shalaby, and M. E. El-Raey (2011), Aerosol climatology over Nile Delta based on MODIS, MISR and OMI satellite data, Atmos. Chem. Phys. Discuss., 11, 1044910484.
  • Markou, M. T., and P. Kassomenos (2010), Cluster analysis of five years of back trajectories arriving in Athens, Greece, Atmos. Res., 98, 438457.
  • Martin, J. H., R. M. Gordon, and S. E. Fitzwater (1991), The case for iron, Limnol. Oceanogr., 36, 17931802.
  • Membery, D. A. (1983), Low level wind profiles during the Gulf Shamal, Weather, 38, 1824.
  • Middleton, N. J. (1986a), Dust storms in the Middle East, J. Arid Environ., 10, 8396.
  • Middleton, N. J. (1986b), A geography of dust storms in south-west Asia, J. Climatol., 6, 183196.
  • Middleton, N. J., and Q. Z. Chaudhary (1988), Severe dust storm at Karachi, 31 May 1986, Weather, 438, 298301.
  • Middleton, N. J., and A. S. Goudie (2001), Saharan dust: Sources and trajectories, Trans. Inst. Br. Geographers NS, 26, 165181.
  • Mohalfi, S., H. S. Bedi, T. N. Krishnamurti, and S. D. Cocke (1998), Impact of snortwave radiative effects of dust aerosols on the summer season heat low over Saudi Arabia, Mon. Weather Rev., 126, 31533168.
  • Moody, J. L. (1986), The influence of meteorology on precipitation chemistry at selected sites in the Eastern United States, Ph.D. dissertation, 176 pp., University of Michigan.
  • Moody, J., and J. Galloway 1988, Quantifying the relationship between atmospheric transport and the chemical composition of precipitation on Bermuda, Tellus, 40B, 436479.
  • Moore, B. J., P. J. Neiman, F. M. Ralph, and F. E. Barthold (2012), Physical processes associated with heavy flooding rainfall in Nashville, Tennessee, and vicinity during 1–2 May 2010: The role of an atmospheric river and mesoscale convective systems, Mon. Weather Rev., 140, 358378.
  • Morales, C. (1979), Saharan Dust. Scope 14, 297 pp., John Wiley & Sons, New York.
  • Park, S. -U., L. -S. Chang, and E. -H. Lee 2005, Direct radiative forcing due to aerosols in East Asia during a Hwangsa (Asian dust) event observed on 19–23 March 2002 in Korea, Atmos. Environ., 39, 25932606.
  • Perrone, T. J. (1979), Winter Shamal in the Persian Gulf. NAVEN-VPREDRSCHFAC, TR 79–06, Naval Research Laboratory, 160 pp. [Available from Naval Research Laboratory, Monterey, CA 93043].
  • Peterson, S. T., and C. E. Junge (1971), Sources of particulate matter in the atmosphere. In Man's Inspection on the Climate. Cambridge, Matthews WH, Kellogg WW, Robinson GD (eds), pp. 310320, M.I.T. Press, Cambridge.
  • Philipp, A., P. M. Della-Marta, J. Jacobeit, D. R. Fereday, P. D. Jones, A. Moberg, and H. Wanner (2007), Long-term variability of daily North Atlantic-European pressure patterns since 1850 classified by simulated annealing clustering, Journal of Climate, 20, 40654095, doi:10.1029/D2002JD002687.
  • Pope, C. A., R. T. Burnett, M. J. Thun, E. E. Calle, D. Krewski, K. Ito, and G.D. Thurston (2002), Lung cancer, cardio-pulmonary mortality and long term exposure to fine particulate air pollution, JAMA, J. Am. Med. Assoc., 287, 11321141, doi:10.1001/jama.287.9.1132.
  • Prasad, A. K., and R. P. Singh (2007), Changes in aerosol parameters during major dust storm events (2001–2005) over the Indo-Gangetic Plains using AERONET and MODIS data, J. Geophys. Res., 112, D09208, doi:10.1029/2006JD007778.
  • Prasad, A. K., H. El-Askary, and M. Kafatos (2010), Implications of high altitude desert dust transport from western Sahara to Nile Delta during biomass burning season, Environ. Pollut., 158, 33853391.
  • Prospero, J. M. (1981), Eolian transport to the world ocean. In: Emiliani C (ed) The Sea: The Oceanic Lithosphere, pp. 801874, John Wiley & Sons, New York.
  • Prospero, J. M. (1996), Saharan dust transport over the Atlantic ocean and the Mediterranean: An overview, in The Impact of Desert Dust Across the Mediterranean., pp. 133–151, Kluver Acad.: Norwell Mass.
  • Prospero, J. M., P. Ginoux, O. Torres, S. E. Nicholson, and T. E. Gill (2002), Environmental characterization of global sources of atmospheric soil dust identified with the Nimbus 7 Total Ozone Mapping Spectrometer (TOMS) absorbing aerosol product, Rev. Geophys., 40(1), 1002, doi:10.1029/2000RG000095.
  • Remer, L. A., et al. (2005), The MODIS aerosol algorithm, products, and validation, J. Atmos. Sci., 62, 947973.
  • Remer, L. A., et al. (2008), Global aerosol climatology from the MODIS satellite sensors, J. Geophys. Res. Atmos., 113, D14S07, doi:10.1029/2007JD007661.
  • Rolph, G. D. (2003), Real-time Environmental Applications and Display sYstem (READY), report, NOAA Air Resour. Lab., Silver Spring, Md. (Available at http://ready.arl.noaa.gov/HYSPLIT_traj.php).
  • Rolph, G. D. (2012), Real-time Environmental Applications and Display sYstem (READY) website (http://ready.arl.noaa.gov). NOAA Air Resources Laboratory, Silver Spring, MD.
  • Rosenfeld, J. E., D. B. Considine, P. E. Meade, J. T. Bacmeister, C.H. Jackman, and M.R. Schoeberl (1997), Stratospheric effects of Mount Pinatubo aerosol studied with a coupled two-dimensional model, J. Geophys. Res., 102, 36493670.
  • Rousseaw, P. (1987), A graphical aid to the interpretation and validation of cluster analysis, J. Comput. Appl. Math., 20, 5365.
  • Salomonson, V. V., W. L. Barnes, P. W. Maymon, H. E. Montgomery, and H. Ostrow (1989), MODIS: Advanced facility instrument for studies of the Earth as a system, IEEE T. Geosci. Remote, 27, 145153.
  • Salvador, S., and P. Chan (November 2004), Determining the number of clusters/segments in hierarchical clustering/segmentation algorithms, in Proceedings of the 16th IEEE International Conference on Tools with Artificial Intelligence (ICTAI ’04), pp. 576–584.
  • Sarthou, G., et al. (2003), Atmospheric iron deposition and sea-surface dissolved iron concentrations in the eastern Atlantic Ocean, Deep Sea Res I, 50, 13391352.
  • Schollaert, S. E., and J. T. Merrill (1998), Cooler sea surface west of the Sahara Desert correlated to dust events, Geophys. Res. Lett., 25, 35293532.
  • Schutz, L., R. Jaenicke, and H. Pietrek (1981), Saharan dust transport over the North Atlantic Ocean (Geological Society of American Special Paper 186). In Desert dust: Origin, characteristic, and effect on man, ed. T.L. Pewe, 87100 pp., Geological Society of America: Boulder, CO.
  • Shao, Y. (2001), A model for mineral dust emission, J. Geophys. Res., 106, 2023920254.
  • Shinn, E. A., G. W. Smith, J. M. Prospero, P. Betzer, M. L. Hayes, V. Garrison, and R.T. Barber (2000), African dust and the demise of Caribbean coral reefs, Geophys. Res. Lett., 27, 3029.
  • Stohl, A. 1998, Computation, accuracy and application of trajectories – A review and bibliography, Atmos. Environ., 32, 947966.
  • Sun, D., K. M. Lau, and M. Kafatos (2008), Contrasting the 2007 and 2005 hurricane seasons: Evidence of possible impacts of Saharan dry air on tropical cyclone activity in the Atlantic basin, Geophys. Res. Lett., 35, L15405, doi:10.1029/2008GL034529.
  • Tanaka, T. Y., et al. (2005), Possible transcontinental dust transport from North Africa and the Middle East to East Asia, Atmos. Environ., 39, 39013909.
  • Tegen, I., A. A. Lacis, and I. Fung (1996), The influence of mineral aerosols from disturbed soils on the global radiation budget, Nature, 380, 419422, doi:10.1038/380419a0.
  • Thalib, L., and A. Al-Taiar (2012), Dust storms and the risk of asthma admissions to hospitals in Kuwait, Sci. Total Environ., 433, 347351.
  • Thiagarajan, N., and C. T. A. Lee (2004), Trace-element evidence for the origin of desert varnish by direct aqueous atmospheric deposition, Earth Planet. Sci. Lett., 224, 131141.
  • Toledano, C., V. E. Cachorro, A. M. de Frutos, B. Torres, A. Berjon, M. Sorribas, and R.S. Stone (2009), Airmass classification and analysis of aerosol types at El Arenosillo (Spain), J. Appl. Meteorol. Climatol., 48, 962981, doi:10.1175/2008JAMC2006.1.
  • Trigo, I. F., T. D. Davies, and G. R. Bigg (1999), Objective climatology of cyclones in the Mediterranean region, J. Climate, 12, 16851696.
  • Valenzuela, A., F. J. Olmo, H. Lyamani, M. Antón, A. Quirantes, and L. Alados-Arboledas (2012), Classification of aerosol radiative properties during African desert dust intrusions over southeastern Spain by sector origins and cluster analysis, J. Geophys. Res., 117, D06214, doi:10.1029/2011JD016885.
  • Vishkaee, F. A., C. Flamant, J. Cuesta, P. Flamant, and H. R. Khalesifard (2011), Multiplatform observations of dust vertical distribution during transport over northwest Iran in the summertime, J. Geophys. Res., 116, D05206, doi:10.1029/2010JD014573.
  • Vishkaee, F. A., C. Flamant, J. Cuesta, L. Oolman, P. Flamant, and H. R. Khalesifard (2012), Dust transport over Iraq and northwest Iran associated with winter Shamal: A case study, J. Geophys. Res., 117, D03201, doi:10.1029/2011JD016339.
  • Washington, R., M. Todd, N. J. Middleton, and A. S. Goudie (2003), Dust-storm source areas determined by the Total Ozone Monitoring Spectrometer and surface observations, Ann. Assoc. Am. Geographers, 93, 297313.
  • Wong, S., and A. E. Dessler (2005), Suppression of deep convection over the tropical North Atlantic by the Saharan air layer, Geophys. Res. Lett., 32, L09808, doi:10.1029/2004GL022295.
  • Wong, S., A. E. Dessler, N. M. Mahowald, P. Yang, and Q. Feng (2009), Maintenance of lower tropospheric temperature inversion in the Saharan air layer by dust and dry anomaly, J. Climate, 22, 51495162.
  • Wu, L. (2007), Impact of Saharan air layer on hurricane peak intensity, Geophys. Res. Lett., 34, L09802, doi:10.1029/2007GL029564.
  • Yong-Seung, C., and Y. Ma-Beong (1996), On the occurrence of yellow sand and atmospheric loadings, Atmos. Environ., 3013, 23872397.
  • Žabkar, R., J. Rakovec, and S. Gaberšec (2008), A trajectory analysis of summertime ozone pollution in Slovenia, Geofizika, 25, 179202.
  • Zhu, X. R., J. M. Prospero, and F. J. Miller (1997), Daily variability of soluble Fe (II) and soluble total Fe in North African dust in the trade winds at Barbados, J. Geophys. Res., 102, D17, 2129721305.