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Glory revealed in disk-integrated photometry of Venus

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arxiv 1406.0277 v1 pith:O6BKTU7X submitted 2014-06-02 astro-ph.EP

classification astro-ph.EP
keywords phaseplanetgloryanglesopticalvenusphotometryproperties
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Context. Reflected light from a spatially unresolved planet yields unique insight into the overall optical properties of the planet cover. Glories are optical phenomena caused by light that is backscattered within spherical droplets following a narrow distribution of sizes; they are well known on Earth as localised features above liquid clouds. Aims. Here we report the first evidence for a glory in the disk-integrated photometry of Venus and, in turn, of any planet. Methods. We used previously published phase curves of the planet that were reproduced over the full range of phase angles with model predictions based on a realistic description of the Venus atmosphere. We assumed that the optical properties of the planet as a whole can be described by a uniform and stable cloud cover, an assumption that agrees well with observational evidence. Results. We specifically show that the measured phase curves mimic the scattering properties of the Venus upper-cloud micron-sized aerosols, also at the small phase angles at which the glory occurs, and that the glory contrast is consistent with what is expected after multiple scattering of photons. In the optical, the planet appears to be brighter at phase angles of 11-13 deg than at full illumination; it undergoes a maximum dimming of up to 10 percent at phases in between. Conclusions. Glories might potentially indicate spherical droplets and, thus, extant liquid clouds in the atmospheres of exoplanets. A prospective detection will require exquisite photometry at the small planet-star separations of the glory phase angles.

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  1. Planet-wide, Concentric Density Waves in Venus's Upper Atmosphere Revealed through Polarimetry?

    astro-ph.EP 2026-07 conditional novelty 7.0 of 10

    Faint concentric rings in Venus's polarized reflected light, seen once in 2010, are plausibly caused by 5-10% density waves in the upper atmosphere above the clouds.

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