Abstract
RECENT radar observations1 and subsequent discussions2,3 indicate that the rotational period of Mercury may be coupled4 to its orbital period in the ratio 2 : 3. Here we examine the insolation and surface temperatures that would result from such coupling and consider some observable consequences.
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References
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SOTER, S., ULRICHS, J. Rotation and Heating of the Planet Mercury. Nature 214, 1315–1316 (1967). https://doi.org/10.1038/2141315a0
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DOI: https://doi.org/10.1038/2141315a0
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