Using the transit of Venus to probe the upper planetary atmosphere
Fabio Reale, Angelo F. Gambino, Giuseppina Micela, Antonio Maggio,, Thomas Widemann, Giuseppe Piccioni

TL;DR
This study uses the 2012 Venus transit observed in multiple high-energy bands to measure the planet's atmospheric layers, revealing ionosphere density and demonstrating a method applicable to exoplanet studies and future missions.
Contribution
It provides the first multi-band high-resolution measurements of Venus's atmospheric radius during transit, highlighting the potential for studying exoplanet atmospheres in high-energy wavelengths.
Findings
Venus's optical radius is about 80 km larger than its solid body radius.
The radius increases by over 70 km in EUV and soft X-ray bands.
Measurements reveal the densest ion layers of Venus's ionosphere.
Abstract
The atmosphere of a transiting planet shields the stellar radiation providing us with a powerful method to estimate its size and density. In particular, because of their high ionization energy, atoms with high atomic number (Z) absorb short-wavelength radiation in the upper atmosphere, undetectable with observations in visible light. One implication is that the planet should appear larger during a primary transit observed in high energy bands than in the optical band. The last Venus transit in 2012 offered a unique opportunity to study this effect. The transit has been monitored by solar space observations from Hinode and Solar Dynamics Observatory (SDO). We measure the radius of Venus during the transit in three different bands with subpixel accuracy: optical (4500A), UV (1600A, 1700A), Extreme UltraViolet (EUV, 171-335A) and soft X-rays (about 10A). We find that, while the Venus…
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