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Snap-shot from a simulation of mantle convection at Ra=10**6. Image displays the isosurfaces of the residual temperature with yellow corresponding to 0.1 (upwelling) and blue corresponding to -0.1 (downwelling). The red solid sphere shows the inner boundary of the 3D shell corresponding to the core. A hybrid radial basis function—pseudospectral method for thermal convection in a 3-D spherical shell.

Just Published

Georgiopoulou, A., D. G. Masson, R. B. Wynn, and S. Krastel (2010),

Sahara Slide: Age, initiation, and processes of a giant submarine slide,

Geochem. Geophys. Geosyst., 11, Q07014, doi:10.1029/2010GC003066

22 pages, 13 figures, 1 table

28 July 2010 [Abstract] [Dynamic Article] [Print PDF]

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Geochemistry, Geophysics, Geosystems (G3) is an electronic journal that publishes research papers on the chemistry, physics, and biology of Earth and planetary processes. Interdisciplinary papers are especially encouraged. G3 seeks original scientific contributions pertaining to understanding the Earth as a system, including observational, experimental, and theoretical investigations of the solid Earth, hydrosphere, atmosphere, and biosphere at all spatial and temporal scales. G3 strives to be at the cutting edge of electronic publishing by encouraging the innovative use of data analysis and visualization formats.

Published by AGU and the Geochemical Society.

Impact Factor 2.626 in the 2009 Journal Citation Reports

ISSN: 1525–2027
CODEN: GGGGFR

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