Numerical simulation of dispersion of volcanic CO2 seeped from seafloor by using multi-scale ocean model

OCEANS'10 IEEE Sydney, OCEANSSYD 2010

Volumn , Issue , 2010, Pages

  Harata, Muneyasu ^a   Sato, Toru ^a   Hirabayashi, Shinichiro ^a   Goto, Koichi ^b  

^a UNIVERSITY OF TOKYO   (Japan)

^b The General Environmental Technos Co Ltd   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

ADVECTION - DIFFUSION; MESOSCALE; MULTISCALES; NUMERICAL SIMULATION; OBSERVED DATA; OCEAN MODEL; SEA FLOOR; SMALL-SCALE MODELS; WATER COLUMNS;

COMPUTER SIMULATION; DISSOLUTION; HYDRAULICS; HYDRODYNAMICS; VOLCANOES;

OCEANOGRAPHY;

EID: 78349267186     PISSN: None     EISSN: None     Source Type: Conference Proceeding    
DOI: 10.1109/OCEANSSYD.2010.5603668     Document Type: Conference Paper

References (7)

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2. T. Sato, K. Tonoki, Y. Tsuchiya, "Numerical and hydraulic simulations of effect of density current generators in semi-enclosed tidal bays", Coastal Engrg. vol. 53, pp. 49-64, 2006.
3. Y. Kano, T. Sato, J. Kita, S. Hirabayashi, S. Tabeta, "Model prediction on the rise of pCO2 in uniform flows by leakage of CO2 purposefully stored under the seabed", Int. J. Greenhouse Gas Control, vol. 3, pp. 617-625, 2009.
4. Pitzer, K.S., Sterner, S.M. 1994. Equations of state valid continuously from zero to extreme pressures for H2O and CO2. Journal of Chemical Physics 101: 3111-3116.
5. Alendal G., Drange, H. 2001. Two-phase, near-field modeling of purposefully released CO2 in the ocean. Journal of Geophysical Research 106(C1): 1085-1096.
6. Smagorinsky, J. 1993. Some historical remarks on the use of nonlinear viscosities. In Galperin, B. and Orszag, S.A. (eds.) Large eddy simulation of complex engineering and geophysical flows. Cambridge University Press. ISBN 0-521-43009-7. pp. 3-36.
7. Y. Kikawada, J. Kosaka, T. Oi, J. Hashimoto, -Chemical compositions of volcanic gases from submarine fumaroles in Wakamiko Caldera, northern Kagoshima Bay, Japan", J. Balneological Soc. Japan, vol. 57, pp.30-41, 2009 (in Japanese).