Árbók VFÍ/TFÍ - 01.06.2010, Síða 250

Heimildir
[1] Arystanbekova, N. K. (2004). Application of Gaussian plume models forairpollution simulation at instantaneous emissions.
Math. Comput. Simul., 67(4-5), 451-458.
[2] Barr, S., og Gifford, F. A. (1987). The random force theory applied to regional scale tropospheric diffusion. Atmos. Environ,
21 (8), 1737-1741.
[3] Briggs, G.A. (1972). Dispersion of chimney plumes in neutral and stable surroundings. Atmos. Environ., 6(1), 507-510.
[4] Bursik,M. I„ Kobs,S. E„ Burns, A„ Braitseva, 0.A„ Bazanova, L. I„ Melekestsev, I.V., Kurbatov, A„ og Pieri, D.C. (2009). Volcanic
plumes and wind: Jetstream interaction examples and implications forairtraffic.l. Volcanol.Geotherm. Res„ 186(1 -2), 60-67.
[5] Csanady, G. T. (1973). Turbulent diffusion in the environment. Geophysical and Astrophysics Monographs, D. Reidel
Publishing Company. Dordrecht, Holland.
[6] deNevers, N. (2000). Airpollution control engineering (2.edition). McGrawHill International. Singapore.
[7] Davies, F„ Middleton, D. R„ og Bozier, K. E. (2007). Urban air pollution modelling and measurements of boundary layet
height. Atmos. Environ., 41 (19), 4040-4049.
[8] Draxler,R.R.,og Hess,G.D.U004).DescriptionoftheHYSPLIT4modelingsystem.NOAATechn\ca\ Memorandum ERL ARL-224,28p.
[9] Eggert Norðdal (2010). Ljósmynd. Sótt 01.09.10 frá www.flickr.com/photos/35133216@N05/
[1 OJEínar Svavarsson (2010).Ljósmynd.Sótt 01.09.2010 frá www.flickr.com/photos/emstrur/
[11 JGifford, F. A. (1982). Horizontal diffusion in the atmosphere - a Lagrangian-dynamicat theory. Atmos. Environ., 16(3), 505-512.
[12] Gifford, F. A. (1984). The random force theory - application to mesco-scaie and iarge-scaie atmospheric diffusion. Bound.-
Layer Meteor., 30(1 -4), 159-175.
[13] Gjevik, B„ Dagestad, K.F., og Johannessen J.A. (2010). Atmospheric lee-wave patterns in the wakes of islands and capes
revealed by moduiations ofsea surface roughness. Proceedings of the RSE-DNVA 2nd Norway-Scotland Internal Wave
Symposium.Edinburgh, United Kingdom,Nov. 1-2.
[14] Glaze, L. S„ og Baloga, S. M. (1996). Sensitivity of buoyant plume heights to ambient atmospheric conditions: Implications
for volcanic eruption columns. J. Geophys. Res.-Atmos„ 101 (D1), 1529-1540.
[15] Jarðvísindastofhun Háskólans og Veðurstofa (slands (2010). Dagleg samatekt um gang eldgossins I Eyjafjallajökli. Sótt af veftiðunum
www.evropusamvinna.is/page/jh_EYJ02010_samantektogwww.vedur.is/skjalftar-og-eldgos/frodleikur/greinar/nr/1863.
[16] Kinoshita, K. (1996). Observation offiow and dispersion of vocanic clouds from Mt. Sakurajima. Atmos. Environ., 30(16),
2831-2837.
[17] Martin, D.O. (1976). The change of concentration standard deviation with distance, J. of the Air Pollution Control
Association, 26 (2), 145-147.
[18] NASA's Earth Observatory (2010). Gervihnattarmyndir. Sótt 20.08.2010 frá earthobservatory.nasa.gov/NaturalHazards/-
event.php?id=43253.
[19] Papp, K. R„ Dean, K. G„ og Dehn, J. (2005). Predicting regions susceptibie to high concentrations ofairborne volcanic ash in
the North Pacific region. J. Volcanol. Geotherm. Res„ 148(3-4), 295-314.
[20] Pisso, l„ Real, E„ Law, K. S„ Legras, B„ Bousserez, N„ Attie, J. L„ og Schlager, H. (2009). Estimation ofmixing in teh troposphete
from Lagrangian trace gas reconstructions during long-range poiiution plume transport. J. Geophys. Res.-Atmos., 114, Art-
No. D19301.
[21 ]Pudykiewicz, J. (1989). Simulation ofthe Chernobyi dispersion with a 3-D hemispheric tracer model.Tellus, 41B, 391 -412.
[22] Searcy, C„ Dean, K„ og Stringer, W. (1998). PUFF:A high resolution volcanic ash tracking model. J. Volcanol. Geotherm. Pes.,
80,1-16.
[23] Sparks, R. S. J„ Bursik, M. I„ Carey, S. N„ Gilbert, J. S.,Glaze, L. S, Sigurdsson H.,og Woods,A.W.(1997). Voicanic piumes. John
Wiley & Sons Ltd, West Sussex, England.
[24] Stunder,BJ.B.,Heffter,J.L.,ogDraxler,R.R.(2007).A/rbornevo/can/cashforecastoreore//ob///ty.WeatherForecast.,22(5),1132-1139-
[25] Tanaka, H. L„ og Yamamoto, K. (2002). Numericalsimulation ofvolcanicplume dispersat from Usu volcano in Japan on3t
March 2000 using PUFFmodel. Earth Planets Space, 54,743-752.
[26] Thorburn, H. (2010) Ljósmynd. Sótt 01.09.2010 frá commons.wikimedia.org/wiki/File:Eyjafjallaj%C3%B6kull_panorama.jpg'
[27] Tiesi, A„ Villani, M.G., D'lsidoro, M„ Prata, A. J„ Maurizi, A„ ogTampieri, F. (2006).Estimation of dispersion coefficient in the
troposphere from satellite images ofvolcanicptume.: Application to Mt. Etna, Italy. Atmos. Environ., 40(4), 628-638.
[28] Tupper, A„ Itikarai, l„ Richards, M„ Prata, F„ Carn, S„ og Rosenfeld, D. (2007). Facing the chailenges ofthe international ait'
ways volcano watch.The 2004/05 eruptions of Manam, Papua New Guinea.Weather and forecasting, 22(1), 175-191-
[29] Turner, D.B. (1994) Workbook of Atmospheric Dispersion Estimates. An introduction to Dispersion Modeling (2nd ed.)
Lewis Publishers.USA.
[30] Tsuang, B. J. (2003). Quantification on the source/receptor relationship of primary poiiutants and secondary aerosols by a
Gaussian plume trajectory model. Part I theory. Atmos. Environ., 37(28), 3981-3991.
[31] University of Wyoming (2010). Loftslagsgögn. Sótt 18.08.2010 frá weather.uwyo.edu/upperair/sounding.html
[32] Veðurstofa fslands. (2010).Radarmyndir, sendar með tölvupósti 23.08.2010.
[33] Webley,P.,og Mastin L. (2009)./mprovedpred/cf/onanc/frac/r/ngofvo/can/casbc/ouds.J.Volcanol.Geotherm.Res., 186(1-2), 1'®’
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Arbók VFl/TFf 2010