Variations in Vertical CO/CO2 Profiles in the Martian Mesosphere and Lower Thermosphere Measured by the ExoMars TGO/NOMAD: Implications of Variations in Eddy Diffusion Coefficient
dc.contributor.author | Yoshida, N. | |
dc.contributor.author | Nakagawa, H. | |
dc.contributor.author | Aoki, S. | |
dc.contributor.author | Erwin, J. | |
dc.contributor.author | Vandaele, A.C. | |
dc.contributor.author | Daerden, F. | |
dc.contributor.author | Thomas, I. | |
dc.contributor.author | Trompet, L. | |
dc.contributor.author | Koyama, S. | |
dc.contributor.author | Terada, N. | |
dc.contributor.author | Neary, L. | |
dc.contributor.author | Murata, I. | |
dc.contributor.author | Villanueva, G. | |
dc.contributor.author | Liuzzi, G. | |
dc.contributor.author | Lopez-Valverde, M.A. | |
dc.contributor.author | Brines, A. | |
dc.contributor.author | Modak, A. | |
dc.contributor.author | Kasaba, Y. | |
dc.contributor.author | Ristic, B. | |
dc.contributor.author | Bellucci, G. | |
dc.contributor.author | López-Moreno, J.J. | |
dc.contributor.author | Patel, M. | |
dc.date | 2022 | |
dc.date.accessioned | 2022-05-31T10:09:43Z | |
dc.date.available | 2022-05-31T10:09:43Z | |
dc.identifier.uri | https://orfeo.belnet.be/handle/internal/9947 | |
dc.description | Abstract Using the Nadir and Occultation for MArs Discovery instrument aboard Trace Gas Orbiter, we derived the CO/CO2 profiles between 75 and 105 km altitude with the equivalent width technique. The derived CO/CO2 profiles showed significant seasonal variations in the southern hemisphere with decreases near perihelion and increases near aphelion. The estimation of the CO/CO2 profiles with a one-dimensional photochemical model shows that an altitude-dependent eddy diffusion coefficient better reproduces the observed profiles than a vertically uniform one. Our estimation suggests that the eddy diffusion coefficient in Ls = 240–270 is uniformly larger by a factor of ∼2 than that in Ls = 90–120 in the southern hemisphere, while they are comparable in the northern hemisphere. This fact demonstrates that the eddy diffusion coefficient is variable with season and latitude. | |
dc.language | eng | |
dc.title | Variations in Vertical CO/CO2 Profiles in the Martian Mesosphere and Lower Thermosphere Measured by the ExoMars TGO/NOMAD: Implications of Variations in Eddy Diffusion Coefficient | |
dc.type | Article | |
dc.subject.frascati | Physical sciences | |
dc.audience | Scientific | |
dc.subject.free | Mars | |
dc.subject.free | eddy diffusion coefficient | |
dc.subject.free | atmospheric composition | |
dc.subject.free | mesosphere | |
dc.subject.free | spectroscopy | |
dc.subject.free | retrieval | |
dc.source.title | Geophysical Research Letters | |
dc.source.volume | 49 | |
dc.source.issue | 10 | |
dc.source.page | e2022GL098485 | |
Orfeo.peerreviewed | Yes | |
dc.identifier.doi | 10.1029/2022GL098485 | |
dc.identifier.scopus |