The Open UniversitySkip to content
 

Global analysis and forecasts of carbon monoxide on Mars

Holmes, James A.; Lewis, Stephen R.; Patel, Manish R. and Smith, Michael D. (2019). Global analysis and forecasts of carbon monoxide on Mars. Icarus, 328 pp. 232–245.

Full text available as:
Full text not publicly available (Accepted Manuscript)
Due to publisher licensing restrictions, this file is not available for public download until 15 March 2020
Click here to request a copy from the OU Author.
DOI (Digital Object Identifier) Link: https://doi.org/10.1016/j.icarus.2019.03.016
Google Scholar: Look up in Google Scholar

Abstract

Spatial and temporal variations in the Martian carbon monoxide (CO) cycle have been investigated through combining Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) retrievals of carbon monoxide mixing ratio and Mars Climate Sounder (MCS) temperature profiles with a Martian global circulation model (GCM) to produce the first global reanalysis of the Martian CO cycle.

The reanalysis reduces the root mean square error between the forecast and CRISM CO retrievals by a factor of 2–4, dependent on the time of year. Forecasts initiated from the reanalysis show an improved match to standalone CRISM CO retrievals from northern winter solstice to northern summer solstice, indicating the benefit of data assimilation in simulating the CO abundance. The northern summer solstice CO minimum between 10∘S – 50∘S in the CRISM CO retrievals is found to be caused by a suppression of CO-enriched air leaking from the Hellas and Argyre basins, and is also strongly influenced by the amount of carbon dioxide condensing at the time. The GCM is the first reported to simulate the local CO minimum however it is weaker in strength, as CO-enriched air is also released northward in the area of Argyre basin in the GCM because of a shifted boundary between the southern polar vortex and mid-latitudes. The reanalysis, as a result of the assimilation of MCS temperature profiles, indicates that the polar vortex boundary is northward of Argyre basin and hence no northerly transport of CO-enriched air should be present over this location.

Differences in local CO abundance between the reanalysis and GCM are also evident in spatio-temporal regions where no nearby CRISM CO retrievals are available as a result of alterations in local circulation and the sublimation/condensation of carbon dioxide through the combined assimilation of CRISM CO retrievals alongside MCS temperature profiles, illustrating how constraints can be imposed indirectly on the CO cycle through the powerful technique of data assimilation.

Item Type: Journal Item
ISSN: 0019-1035
Project Funding Details:
Funded Project NameProject IDFunding Body
Not SetST/R001405/1UK Space Agency (UKSA)
Not SetST/P001262/1UK Space Agency (UKSA)
Not SetST/S00145X/1UK Space Agency (UKSA)
Mars Reconnaissance Orbiter ProjectNot SetNot Set
Keywords: Mars; Atmosphere; Data assimilation; Atmospheres; Chemistry
Academic Unit/School: Faculty of Science, Technology, Engineering and Mathematics (STEM) > Physical Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM)
Item ID: 60177
Depositing User: ORO Import
Date Deposited: 28 Mar 2019 13:35
Last Modified: 14 Nov 2019 13:21
URI: http://oro.open.ac.uk/id/eprint/60177
Share this page:

Metrics

Altmetrics from Altmetric

Citations from Dimensions

Actions (login may be required)

Policies | Disclaimer

© The Open University   contact the OU