A volcanically active planet is shown in closeup at the left side of the image with glowing eruptions and lines of lava on the surface. To the right and in the distance is a faint blue glowing ball representing the more massive planet in the system.Sixteen frames from Voyager 1's flyby of Jupiter in 1979 were merged to create this image. Jupiter's Great Red Spot is visible in the center. Jupiter's moon Europa can be seen in the foreground at the bottom left of the image.The frame is a horizontal rainbow of color on a grid. Shadows of molecules can be seen through the light as well as the jagged peaks and troughs of spectral lines.
Fizzy Super Earths and Lava Worlds“Fizzy Super-Earths: Impacts of Magma Composition on the Bulk Density and Structure of Lava Worlds.” in The Astrophysical Journal.01/03
Identifying Hydrothermal Activity on Icy Ocean Worlds“Ethene-ethanol ratios as potential indicators of hydrothermal activity at Enceladus, Europa, and other icy ocean worlds.” In Icarus.02/03
NASA Raman Spectroscopic Database"The NASA Raman spectroscopic database: Ramdb version 1.00.” In Icarus.03/03
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June 2011Hydromagnetic waves in weakly-ionized media - I. Basic theory, and application to interstellar molecular clouds

Mouschovias, T. C., Ciolek, G. E., & Morton, S. A. (2011). Monthly Notices of the Royal Astronomical Society, 415(2), 1751–1782. doi:10.1111/j.1365-2966.2011.18817.x

Precise Stellar Radial Velocities of an M Dwarf with a Michelson Interferometer and a Medium-Resolution Near-Infrared Spectrograph

Muirhead, P. S., Edelstein, J., Erskine, D. J., Wright, J. T., Muterspaugh, M. W., Covey, K. R., … Wishnow, E. H. (2011). Publications of the Astronomical Society of the Pacific, 123(904), 709–724. doi:10.1086/660802

Stratospheric superrotation in the TitanWRF model

Newman, C. E., Lee, C., Lian, Y., Richardson, M. I., & Toigo, A. D. (2011). Icarus, 213(2), 636–654. doi:10.1016/j.icarus.2011.03.025

THE PHOTOEVAPORATIVE WIND FROM THE DISK OF TW Hya

Pascucci, I., Sterzik, M., Alexander, R. D., Alencar, S. H. P., Gorti, U., Hollenbach, D., … Owen, J. (2011). The Astrophysical Journal, 736(1), 13. doi:10.1088/0004-637x/736/1/13

Greenhouse warming by nitrous oxide and methane in the Proterozoic Eon

Roberson, A. L., Roadt, J., Halevy, I., & Kasting, J. F. (2011). Geobiology, 9(4), 313–320. doi:10.1111/j.1472-4669.2011.00286.x

Earth as an Extrasolar Planet: Earth Model Validation Using EPOXI Earth Observations

Robinson, T. D., Meadows, V. S., Crisp, D., Deming, D., A'Hearn, M. F., Charbonneau, D., … Livengood, T. A. (2011). Astrobiology, 11(5), 393–408. doi:10.1089/ast.2011.0642

Biogenicity of Apex Chert microstructures

Schopf, J. W., & Kudryavtsev, A. B. (2011). Nature Geosci, 4(6), 346–347. doi:10.1038/ngeo1172

Large Sulfur Isotope Fractionation Does Not Require Disproportionation

Sim, M. S., Bosak, T., & Ono, S. (2011). Science, 333(6038), 74–77. doi:10.1126/science.1205103

A low mass for Mars from Jupiter’s early gas-driven migration

Walsh, K. J., Morbidelli, A., Raymond, S. N., O'Brien, D. P., & Mandell, A. M. (2011). Nature, 475(7355), 206–209. doi:10.1038/nature10201

Environmental Conditions Constrain the Distribution and Diversity of Archaeal merA in Yellowstone National Park, Wyoming, U.S.A.

Wang, Y., Boyd, E., Crane, S., Lu-Irving, P., Krabbenhoft, D., King, S., … Dighton, J. (2011). Microbial Ecology, 62(4), 739–752. doi:10.1007/s00248-011-9890-z