Exoplanet HD 209458 b
- October 11th, 2011
- By Paul Anthony Wilson
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Astronomers are not able to obtain the transmission spectra of all the Hot Jupiters discovered thus far. With today’s instruments there are about 10 good targets that allow for transmission-based atmospheric detections (Sing et al. 2009b). These stars, which allow for transmission spectroscopy to be done, have the following attributes in common. Either they orbit a bright host star which in turn gives a better signal to noise (S/N), or they orbit a smaller star which leads to a deeper transit, providing a larger planet-to-star contrast. Also if the exoplanet has a large atmosphere (lower surface gravity, higher effective temperature) it is also easier to detect. Of all the Hot Jupiters discovered thus far, two planets stand out as being the easiest to measure, HD209458b and HD189733b. Almost everything known about Hot Jupiters to this date, comes from the study of these two planets.
HD 209458 b has been the subject of intense study since the first planetary transits were detected (Charbonneau et al. 2000, Henry et al. 2000, Mazeh et al. 2000). It was the first planet to have it’s atmosphere detected using transmission spectroscopy (Charbonneau et al. 2002). What Charbonneau et al. (2002) detected was absorption from sodium which caused a 0.02% deeper light curve relative to simultaneous observations of the transit in adjacent bands. The presence of sodium was later confirmed by Snellen et al. (2008) who used a ground based telescope (Subaru Telescope). Despite this sodium detection, it was not as deep as predicted by a model which assumed a cloudless planetary atmosphere with a solar abundance of sodium. This lead to number of theories such as there being a low primordial abundance of sodium and/or clouds present in the upper atmosphere, to mention a few. Later Rowe et al. (2008) showed that HD 209458 b had a significantly lower albedo than Jupiter using the MOST (Microvariablity and Oscillations of Stars) satellite. This ruled out the presence of bright reflective clouds in the atmosphere. It is now thought that a low sodium abundance is due to condensation (where sodium condenses into sodium sulfide) or ionisation. This is supported by the observation of a sudden abundance change of sodium from the lower atmosphere (where the abundance is about 2 times the solar abundance) to the upper atmosphere (where it is about 0.2 times that of the solar abundance) (Sing et al. 2008). Recent discoveries include the the presence of water in the atmosphere (Beaulieu et al. 2010) and as well as atomic hydrogen, oxygen, and ionized carbon in the upper atmosphere (Koskinen et al. 2010).







Credit: Swinburne Astronomy Productions
Credit: NASA
Credit: NASA
Credit: STSCI