Copy the page URI to the clipboard
Brown, M. A. J.; Patel, M. R.; Lewis, S. R.; Holmes, J. A.; Lefèvre, F.; Mason, J. P. and Crismani, M.
(2024).
DOI: https://doi.org/10.1029/2024je008302
Abstract
Ozone simulated in Mars Global Climate Models (MGCMs) is used to assess the underlying chemistry occurring in the atmosphere. Currently, ozone total column abundance (TCA) is under‐predicted in MGCMs by up to 120%, implying missing or inaccurate chemistry in models. Heterogeneous reactions of hydroxyl radicals (HOX) have been offered as an explanation for some of this bias, because they cause ozone to increase at locations where it's currently under‐predicted. We use four simulations to compare modeled ozone TCA with observations from the UVIS spectrometer aboard the ExoMars Trace Gas Orbiter to improve the representation of heterogeneous processes and their impact on ozone. We use a gas‐phase only run, a dissociative scheme, an adsorbed HOX retention scheme, and a hybrid scheme that combines the dissociative mechanism with the retention of HOX on water ice. We find retention of HOX is dependent on water ice sublimation, and ozone abundance increases when water ice persists for longer periods (1–20 sols). Over time, the loss of HOX causes a depletion in H2O2 concentration (HOX reservoir), and thus allows ozone concentration to increase. When adsorbed HOX are desorbed and dissociate into other by‐products, HOX are not immediately available to destroy ozone. This results in larger ozone concentrations than if desorbed HOX are released directly back into their gaseous states. When using the hybrid scheme, ozone TCA is increased up to 50% where the ozone deficit is greatest, demonstrating the best agreement with observations, and implying that HOX radicals are both retained when adsorbed and dissociate.
Plain Language Summary
Ozone is a trace gas in the martian atmosphere, sensitive to chemical andlight‐induced reactions. This makes it ideal for assessing the underlying reactions for chemical species calledhydroxyl radicals, which destroy ozone and would otherwise be too reactive and shortlived to be measureddirectly. There has been an under‐prediction of ozone in global climate models which implies missing orinaccurate reactions. Heterogeneous reactions (a reaction which includes two or more phases) have beensuggested to fill the deficit in modeled ozone. This involves hydroxyl radicals adsorbing onto water ice, whichcauses ozone to increase. We look at different simulations to understand hydroxyl radical chemistry on thesurface of water ice by comparing to observations from the ExoMars Trace Gas Orbiter. We run four climatemodel simulations to test different theories as to what is occurring at the surface. There are two theories (a)reactions happen at the surface which alter hydroxyl radicals into other chemicals, and (b) hydroxyl radicals stayadsorbed onto water ice for as long as the ice persists. When we combine these theories, we have a more accurateprediction of ozone, which we can then use to infer what happens at the surface.
CORE (COnnecting REpositories)
CORE (COnnecting REpositories)
