BEGIN:VCALENDAR VERSION:2.0 PRODID:-//CERN//INDICO//EN BEGIN:VEVENT SUMMARY:Uncovering 3D variations in the temperature chemistry\, and winds on ultra-hot Jupiters: Targeting multiple species with high-resolution spe ctroscopy DTSTART;VALUE=DATE-TIME:20220908T124500Z DTEND;VALUE=DATE-TIME:20220908T130000Z DTSTAMP;VALUE=DATE-TIME:20241101T160823Z UID:indico-contribution-118@meetings.aip.de DESCRIPTION:Speakers: Joost Wardenier (University of Oxford)\nUltra-hot Ju piters are tidally locked gas giants with dayside temperatures high enough to dissociate hydrogen and other molecules. Featuring sharp chemical grad ients and large temperature contrasts\, their atmospheres are vastly non-u niform. In recent years\, the wealth of data from high-resolution spectrog raphs such as HARPS-N\, CRIRES\, ESPRESSO and IGRINS has yielded spectacul ar insights into the chemical inventory\, wind profiles and temperature st ructures of ultra-hot Jupiters. In particular\, high-precision observation s with ESPRESSO were able to sample the varying Doppler shift of the absor ption lines in the spectrum of a transiting exoplanet.\n\nIn this talk\, I will present a new framework for computing time-dependent\, 3D transit sp ectra of exoplanets at high spectral resolution. We post-process the outpu t of a state-of-the-art global circulation model (the SPART/MITgcm) throug h a GPU-optimised Monte-Carlo radiative transfer code\, called gCMCRT. Thi s allows us to correctly model the millions of spectral lines that can be observed with ground-based instruments\, while accounting for the complex effects of thermal and chemical inhomogeneities\, wind gradients and plane t rotation in a unified framework.\n\nI will demonstrate that different ch emical species\, such as water\, CO\, and iron\, are distributed different ly throughout the atmosphere of an ultra-hot Jupiter\, resulting in unique transit signals for certain atoms and molecules. This is because thermal dissociation and condensation impact the chemical composition of the daysi de and the nightside of the planet. I will show that our framework can qua litatively reproduce the time-dependent iron signal observed by Ehrenreich + (2020) for WASP-76b. To this end\, we either assume that iron condenses into clouds on the nightside\, or that the morning limb is substantially c ooler than expected. \n\nIn addition\, I will illustrate how signals from other species\, such as water (which is dissociated on the dayside) and CO (which is unaffected by temperature) can be used to bypass the inherent d egeneracies associated with the observation of a single species. Finally\, I will cover the results of our recent transit observations of WASP-121b with Gemini-S/IGRINS. These observations targeted water and CO absorption in the infrared\, with the objective to obtain a similar signal-to-noise r atio as the WASP-76b iron signal observed with ESPRESSO. I will discuss ho w interpreting the absorption signals of these three chemical species (wat er\, CO\, iron) within the same framework allows us to place important con straints on the 3D structure of the limb of an ultra-hot Jupiter.\n\nhttps ://iaus379.aip.de/event/16/contributions/118/ LOCATION:Leibniz Institute for Astrophysics Potsdam (AIP) Lecture Hall URL:https://iaus379.aip.de/event/16/contributions/118/ END:VEVENT END:VCALENDAR