Solar cycle variations in mesospheric carbon monoxide

dc.contributor.authorLee, Jae
dc.contributor.authorWu, Dong L.
dc.contributor.authorRuzmaikin, Alexander
dc.contributor.authorFontenla, Juan
dc.date.accessioned2022-03-14T14:05:21Z
dc.date.available2022-03-14T14:05:21Z
dc.date.issued2018-05
dc.description.abstractAs an extension of Lee et al. (2013), solar cycle variation of carbon monoxide (CO) is analyzed with MLS observation, which covers more than thirteen years (2004–2017) including maximum of solar cycle 24. Being produced primarily by the carbon dioxide (CO₂) photolysis in the lower thermosphere, the variations of the mesospheric CO concentration are largely driven by the solar cycle modulated ultraviolet (UV) variation. This solar signal extends down to the lower altitudes by the dynamical descent in the winter polar vortex, showing a time lag that is consistent with the average descent velocity. To characterize a global distribution of the solar impact, MLS CO is correlated with the SORCE measured total solar irradiance (TSI) and UV. As high as 0.8 in most of the polar mesosphere, the linear correlation coefficients between CO and UV/TSI are more robust than those found in the previous work. The photochemical contribution explains most (68%) of the total variance of CO while the dynamical contribution accounts for 21% of the total variance at upper mesosphere. The photochemistry driven CO anomaly signal is extended in the tropics by vertical mixing. The solar cycle signal in CO is further examined with the Whole Atmosphere Community Climate Model (WACCM) 3.5 simulation by implementing two different modeled Spectral Solar Irradiances (SSIs): SRPM 2012 and NRLSSI. The model simulations underestimate the mean CO amount and solar cycle variations of CO, by a factor of 3, compared to those obtained from MLS observation. Different inputs of the solar spectrum have small impacts on CO variation.en_US
dc.description.sponsorshipThis work is supported by NASA Sun-climate research at Goddard Space Flight Center. We would like to thank two anonymous reviewers for valuable comments and suggestions that led to an improved manuscript. We thank the Aura MLS, SORCE, NRLSSI teams for providing their data support, and Jerry Harder and Marty Snow for valuable science discussions.en_US
dc.description.urihttps://www.sciencedirect.com/science/article/pii/S1364682617305606?via%3Dihuben_US
dc.format.extent14 pagesen_US
dc.genrejournal articlesen_US
dc.identifierdoi:10.13016/m2pnk2-lapv
dc.identifier.citationLee, Jae N. Solar cycle variations in mesospheric carbon monoxide. Journal of Atmospheric and Solar-Terrestrial Physics 170 (May 2018) pp 21-3. https://doi.org/10.1016/j.jastp.2018.02.001en_US
dc.identifier.urihttps://doi.org/10.1016/j.jastp.2018.02.001
dc.identifier.urihttp://hdl.handle.net/11603/24380
dc.language.isoen_USen_US
dc.publisherElsevieren_US
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Joint Center for Earth Systems Technology
dc.relation.ispartofUMBC Faculty Collection
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.en_US
dc.rightsPublic Domain Mark 1.0*
dc.rights.urihttp://creativecommons.org/publicdomain/mark/1.0/*
dc.titleSolar cycle variations in mesospheric carbon monoxideen_US
dc.typeTexten_US
dcterms.creatorhttps://orcid.org/0000-0001-9814-9855en_US

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