Articles | Volume 23, issue 2
https://doi.org/10.5194/acp-23-1705-2023
https://doi.org/10.5194/acp-23-1705-2023
Research article
 | 
31 Jan 2023
Research article |  | 31 Jan 2023

Aura/MLS observes and SD-WACCM-X simulates the seasonality, quasi-biennial oscillation and El Niño–Southern Oscillation of the migrating diurnal tide driving upper mesospheric CO primarily through vertical advection

Cornelius Csar Jude H. Salinas, Dong L. Wu, Jae N. Lee, Loren C. Chang, Liying Qian, and Hanli Liu

Related authors

A machine-learning-based marine atmosphere boundary layer (MABL) moisture profile retrieval product from GNSS-RO deep refraction signals
Jie Gong, Dong L. Wu, Michelle Badalov, Manisha Ganeshan, and Minghua Zheng
Atmos. Meas. Tech., 18, 4025–4043, https://doi.org/10.5194/amt-18-4025-2025,https://doi.org/10.5194/amt-18-4025-2025, 2025
Short summary
New insights into the polar ozone and water vapor, radiative effects, and their connection to the tides in the mesosphere–lower thermosphere during major sudden stratospheric warming events
Guochun Shi, Hanli Liu, Masaki Tsutsumi, Njål Gulbrandsen, Alexander Kozlovsky, Dimitry Pokhotelov, Mark Lester, Christoph Jacobi, Kun Wu, and Gunter Stober
Atmos. Chem. Phys., 25, 9403–9430, https://doi.org/10.5194/acp-25-9403-2025,https://doi.org/10.5194/acp-25-9403-2025, 2025
Short summary
A comparison of modeled daytime E-regions from E-PROBED and PyIRI with ionosonde observations
Daniel J. Emmons, Cornelius Csar Jude H. Salinas, Dong L. Wu, Nimalan Swarnalingam, Eugene V. Dao, Jorge L. Chau, Yosuke Yamazaki, Kyle E. Fitch, and Victoriya V. Forsythe
EGUsphere, https://doi.org/10.5194/egusphere-2025-3731,https://doi.org/10.5194/egusphere-2025-3731, 2025
This preprint is open for discussion and under review for Annales Geophysicae (ANGEO).
Short summary
Ozone recovery effects on mesospheric dynamics in the southern hemisphere
Ales Kuchar, Gunter Stober, Dimitry Pokhotelov, Huixin Liu, Han-Li Liu, Manfred Ern, Damian Murphy, Diego Janches, Tracy Moffat-Griffin, Nicholas Mitchell, and Christoph Jacobi
EGUsphere, https://doi.org/10.5194/egusphere-2025-2827,https://doi.org/10.5194/egusphere-2025-2827, 2025
This preprint is open for discussion and under review for Annales Geophysicae (ANGEO).
Short summary
Impacts of Increasing CO2 on Diurnal Migrating Tide in the Equatorial Lower Thermosphere
Masaru Kogure, In-Sun Song, Huixin Liu, and Han-Li Liu
EGUsphere, https://doi.org/10.5194/egusphere-2025-3303,https://doi.org/10.5194/egusphere-2025-3303, 2025
This preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).
Short summary

Cited articles

Akmaev, R. A. and Shved, G. M.: Modelling of the composition of the lower thermosphere taking account of the dynamics with applications to tidal variations of the [OI] 5577 Å airglow, J. Atmos. Terr. Phys., 42, 705–716, 1980. 
Allen, D. R., Stanford, J. L., López-Valverde, M. A., Nakamura, N., Lary, D. J., Douglass, A. R., Cerniglia, M. C., Remedios, J. J., and Taylor, F. W.: Observations of middle atmosphere CO from the UARS ISAMS during the early northern winter 1991/92, J. Atmos. Sci., 56, 563–583, 1999. 
Allen, D. R., Stanford, J. L., Nakamura, N., Lopez-Valverde, M. A., Lopez-Puertas, M., Taylor, F. W., and Remedios, J.J.: Antarctic polar descent and planetary wave activity observed in ISAMS CO from April to July 1992, Geophys. Res. Lett., 27, 665–668, 2000. 
Angelats i Coll, M. and Forbes, J. M.: Dynamical influences on atomic oxygen and 5577 Å emission rates in the lower thermosphere, Geophys. Res. Lett., 25, 461–464, 1998. 
Brasseur, G. P. and Solomon, S.: Aeronomy of the middle atmosphere: Chemistry and physics of the stratosphere and mesosphere, vol. 32, Springer Science & Business Media, https://doi.org/10.1007/1-4020-3824-0_3, 2006. 
Download
Short summary
Upper mesospheric carbon monoxide's (CO) photochemical lifetime is longer than dynamical timescales. This work uses satellite observations and model simulations to establish that the migrating diurnal tide and its seasonal and interannual variabilities drive CO primarily through vertical advection. Vertical advection is a transport process that is currently difficult to observe. This work thus shows that we can use CO as a tracer for vertical advection across seasonal and interannual timescales.
Share
Altmetrics
Final-revised paper
Preprint