Articles | Volume 24, issue 23
https://doi.org/10.5194/acp-24-13299-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-24-13299-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The impact of quasi-biennial oscillation (QBO) disruptions on diurnal tides over the low- and mid-latitude mesosphere and lower thermosphere (MLT) region observed by a meteor radar chain
Jianyuan Wang
National Key Laboratory of Electromagnetic Environment, China Research Institute of Radiowave Propagation, Qingdao 266107, China
Kunming Electro-magnetic Environment Observation and Research Station, Qujing 655500, China
CAS Key Laboratory of Geospace Environment, Department of Geophysics and Planetary Sciences, University of Science and Technology of China, Hefei, China
CAS Center for Excellence in Comparative Planetology, Anhui Mengcheng Geophysics National Observation and Research Station, University of Science and Technology of China, Hefei, China
National Key Laboratory of Electromagnetic Environment, China Research Institute of Radiowave Propagation, Qingdao 266107, China
Kunming Electro-magnetic Environment Observation and Research Station, Qujing 655500, China
CAS Key Laboratory of Geospace Environment, Department of Geophysics and Planetary Sciences, University of Science and Technology of China, Hefei, China
CAS Center for Excellence in Comparative Planetology, Anhui Mengcheng Geophysics National Observation and Research Station, University of Science and Technology of China, Hefei, China
CAS Key Laboratory of Geospace Environment, Department of Geophysics and Planetary Sciences, University of Science and Technology of China, Hefei, China
CAS Center for Excellence in Comparative Planetology, Anhui Mengcheng Geophysics National Observation and Research Station, University of Science and Technology of China, Hefei, China
Hefei National Laboratory, University of Science and Technology of China, Hefei, China
Collaborate Innovation Center of Astronautical Science and Technology, Harbin 150001, China
Iain M. Reid
ATRAD Pty Ltd., Adelaide, SA 5032, Australia
School of Physical Sciences, University of Adelaide, Adelaide, SA 5005, Australia
Jianfei Wu
CAS Key Laboratory of Geospace Environment, Department of Geophysics and Planetary Sciences, University of Science and Technology of China, Hefei, China
CAS Center for Excellence in Comparative Planetology, Anhui Mengcheng Geophysics National Observation and Research Station, University of Science and Technology of China, Hefei, China
Hailun Ye
CAS Key Laboratory of Geospace Environment, Department of Geophysics and Planetary Sciences, University of Science and Technology of China, Hefei, China
CAS Center for Excellence in Comparative Planetology, Anhui Mengcheng Geophysics National Observation and Research Station, University of Science and Technology of China, Hefei, China
Jian Li
CAS Key Laboratory of Geospace Environment, Department of Geophysics and Planetary Sciences, University of Science and Technology of China, Hefei, China
CAS Center for Excellence in Comparative Planetology, Anhui Mengcheng Geophysics National Observation and Research Station, University of Science and Technology of China, Hefei, China
Zonghua Ding
National Key Laboratory of Electromagnetic Environment, China Research Institute of Radiowave Propagation, Qingdao 266107, China
Kunming Electro-magnetic Environment Observation and Research Station, Qujing 655500, China
Jinsong Chen
National Key Laboratory of Electromagnetic Environment, China Research Institute of Radiowave Propagation, Qingdao 266107, China
Kunming Electro-magnetic Environment Observation and Research Station, Qujing 655500, China
Guozhu Li
Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
Yaoyu Tian
National Key Laboratory of Electromagnetic Environment, China Research Institute of Radiowave Propagation, Qingdao 266107, China
Boyuan Chang
National Key Laboratory of Electromagnetic Environment, China Research Institute of Radiowave Propagation, Qingdao 266107, China
Jiajing Wu
National Key Laboratory of Electromagnetic Environment, China Research Institute of Radiowave Propagation, Qingdao 266107, China
Lei Zhao
National Key Laboratory of Electromagnetic Environment, China Research Institute of Radiowave Propagation, Qingdao 266107, China
Kunming Electro-magnetic Environment Observation and Research Station, Qujing 655500, China
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Cited articles
Andrews, D. G., Holton, J. R., and Leovy, C. B.: Middle atmosphere dynamics, Academic Press Inc., 489 pp., https://doi.org/10.1002/qj.49711548612, 1987.
Baldwin, M. P., Gray, L. J., Dunkerton, T. J., Hamilton, K., Haynes, P. H., Randel, W. J., Holton, J. R., Alexander, M. J., Hirota, I., Horinouchi, T., Jones, D. B. A., Kinnersley, J. S., Marquardt, C., Sato, K., and Takahashi, M.: The quasi-biennial oscillation, Rev. Geophys., 39, 179–229, https://doi.org/10.1029/1999RG000073, 2001.
Barton, C. A. and McCormack, J. P.: Origin of the 2016 QBO disruption and its relationship to extreme El Niño events, Geophys. Res. Lett., 44, 11150–11157, https://doi.org/10.1002/2017GL075576, 2017.
Beres, J. H., Garcia, R. R., Boville, B. A., and Sassi, F.: Implementation of a gravity wave source spectrum parameterization dependent on the properties of convection in the Whole Atmosphere Community Climate Model (WACCM), J. Geophys. Res., 110, D10108, https://doi.org/10.1029/2004JD005504, 2015.
Butchart, N.: The Brewer-Dobson circulation, Rev. Geophys., 52, 157–184, https://doi.org/10.1002/2013RG000448, 2014.
Cen, Y., Yang, C., Li, T., Russell III, J. M., and Dou, X.: Suppressed migrating diurnal tides in the mesosphere and lower thermosphere region during El Niño in northern winter and its possible mechanism, Atmos. Chem. Phys., 22, 7861–7874, https://doi.org/10.5194/acp-22-7861-2022, 2022.
Chapman, S. and Lindzen, R.: Atmospheric tides – thermal and gravitational, D. Reidel Publishing Company, Dordrecht, the Netherlands, ISBN 978-94-010-3401-2, 1970.
Collimore, C. C., Martin, D. W., Hitchman, M. H., Huesmann, A., and Waliser, D. E.: On the relationship between the QBO and tropical deep convection, J. Climate, 16, 2552–2568, https://doi.org/10.1175/1520-0442(2003)016<2552:OTRBTQ>2.0.CO;2, 2003.
Coy, L., Newman, P. A., Pawson, S., and Lait, L. R.: Dynamics of the disrupted 2015/16 quasi-biennial oscillation, J. Climate, 30, 5661–5674, https://doi.org/10.1175/jcli-d-16-0663.1, 2017.
Davis, R. N., Du, J., Smith, A. K., Ward, W. E., and Mitchell, N. J.: The diurnal and semidiurnal tides over Ascension Island (° S, 14° W) and their interaction with the stratospheric quasi-biennial oscillation: studies with meteor radar, eCMAM and WACCM, Atmos. Chem. Phys., 13, 9543–9564, https://doi.org/10.5194/acp-13-9543-2013, 2013.
Ebdon, R. A.: Notes on the wind flow at 50 mb in tropical and sub-tropical regions in January 1957 and January 1958, Q. J. Roy. Meteorol. Soc., 86, 540–542, https://doi.org/10.1002/qj.49708637011, 1960.
Ern, M., Diallo, M. A., Khordakova, D., Krisch, I., Preusse, P., Reitebuch, O., Ungermann, J., and Riese, M.: The quasi-biennial oscillation (QBO) and global-scale tropical waves in Aeolus wind observations, radiosonde data, and reanalyses, Atmos. Chem. Phys., 23, 9549–9583, https://doi.org/10.5194/acp-23-9549-2023, 2023.
Ern, M., Ploeger, F., Preusse, P., Gille, J. C., Gray, L. J., Kalisch, S., Mlynczak, M. G., Russell III, J. M., and Riese, M.: Interaction of gravity waves with the QBO: A satellite perspective, J. Geophys. Res.-Atmos., 119, 2329–2355, https://doi.org/10.1002/2013JD020731, 2014.
Gasperini, F.: SD WACCM-X v2.1, National Center for Atmospheric Research [data set], https://doi.org/10.26024/5b58-nc53, 2024.
Geller, M. A., Zhou, T., and Yuan, W.: The QBO, gravity waves forced by tropical convection, and ENSO, J. Geophys. Res.-Atmos., 121, 8886–8895, https://doi.org/10.1002/2015jd024125, 2016.
ray, L. J. and Chipperfield, M. P.: On the interannual variability of trace gases in the middle atmosphere, Geophys. Res. Lett., 17, 933–936, https://doi.org/10.1029/GL017i007p00933, 1990.
Hagan, M. E., Burrage, M. D., Forbes, J. M., Hackney, J., Randel, W. J., and Zhang, X.: QBO effects on the diurnal tide in the upper atmosphere, Earth Planet. Space, 51, 571–578, https://doi.org/10.1186/bf03353216, 1999.
Hampson, J. and Haynes, P.: Influence of the equatorial QBO on the extratropical stratosphere, J. Atmos. Sci., 63, 936–951, https://doi.org/10.1175/jas3657.1, 2006.
He, Y., Zhu, X., Sheng, Z., He, M., and Feng, Y.: Observations of inertia gravity waves in the western Pacific and their characteristic in the 2015/2016 quasi-biennial oscillation disruption, J. Geophys. Res.-Atmos., 127, e2022JD037208, https://doi.org/10.1029/2022JD037208, 2022.
He, M., Forbes, J. M., Jacobi, C., Li, G., Liu, L., Stober, G., and Wang, C.: Observational verification of high-order solar tidal harmonics in the Earth's atmosphere, Geophys. Res. Lett., 51, e2024GL108439, https://doi.org/10.1029/2024GL108439, 2024.
Hersbach, H. and Dee, D.: ERA5 reanalysis is in production, ECMWF Newsletter 147, ECMWF, Reading, UK [dataset], https://www.ecmwf.int/en/newsletter/147/news/era5-reanalysis-production (last access: 31 May 2024), 2016.
Hersbach, H., Bell, B., Berrisford, P., Hirahara, S., Horanyi, A., Munoz-Sabater, J., Nicolas, J., Peubey, C., Radu, R., Schepers, D., Simmons, A., Soci, C., Abdalla, S., Abellan, X., Balsamo, G., Bechtold, P., Biavati, G., Bidlot, J., Bonavita, M., Chiara, G. D., Dahlgren, P., Dee, D., Diamantakis, M., Dragani, R., Flemming, J., Forbes, R., Fuentes, M., Geer, A., Haimberger, L., Healy, S., Hogan, R. J., Holm, E., Janiskova, M., Keeley, S., Laloyaux, P., Lopez, P., Vamborg, C., Villaume, S., and Thepaut, J.-N.: The ERA5 global reanalysis, Q. J. Roy. Meteorol. Soc., 146, 1999–2049, https://doi.org/10.1002/qj.3803, 2020.
Hersbach, H., Bell, B., Berrisford, P., Biavati, G., Horányi, A., Muñoz Sabater, J., Nicolas, J., Peubey, C., Radu, R., Rozum, I., Schepers, D., Simmons, A., Soci, C., Dee, D., and Thépaut, J.-N.: ERA5 monthly averaged data on pressure levels from 1940 to present, Copernicus Climate Change Service (C3S) Climate Data Store (CDS) [data set], https://doi.org/10.24381/cds.6860a573, 2023.
Holdsworth, D. A., Reid, I. M., and Cervera, M. A.: Buckland Park all-sky interferometric meteor radar, Radio Sci., 39, RS5009, https://doi.org/10.1029/2003RS003014, 2004.
Holton, J. R. and Tan, H.-C.: The influence of the equatorial quasi-biennial oscillation on the global circulation at 50 mb, J. Atmos. Sci., 37, 2200–2208, https://doi.org/10.1175/1520-0469(1980)037<2200:tioteq>2.0.co;2, 1980.
Hurrell, J. W., Hack, J. J., Phillips, A. S., Caron, J., and Yin, J.: The dynamical simulation of the Community Atmosphere Model version 3 (CAM3), J. Climate, 19, 2162–2183, https://doi.org/10.1175/JCLI3762.1, 2006.
John, S. R. and Kumar, K. K.: TIMED/SABER observations of global gravity wave climatology and their interannual variability from stratosphere to mesosphere lower thermosphere, Clim. Dynam., 39, 1489–1505, https://doi.org/10.1007/s00382-012-1329-9, 2012.
Kang, M.-J., Chun, H.-Y., and Garcia, R. R.: Role of equatorial waves and convective gravity waves in the 2015/16 quasi-biennial oscillation disruption, Atmos. Chem. Phys., 20, 14669–14693, https://doi.org/10.5194/acp-20-14669-2020, 2020.
Kang, M.-J. and Chun, H.-Y.: Contributions of equatorial waves and small-scale convective gravity waves to the 2019/20 quasi-biennial oscillation (QBO) disruption, Atmos. Chem. Phys., 21, 9839–9857, https://doi.org/10.5194/acp-21-9839-2021, 2021.
Kang, M.-J., Chun, H.-Y., Son, S.-W., Garcia, R. R., An, S., and Park, S.: Role of tropical lower stratosphere winds in quasi-biennial oscillation disruptions, Sci. Adv., 8, eabm7229, https://doi.org/10.1126/sciadv.abm7229, 2022.
Kerzenmacher, T. and Braesicke, P.: QBO: monthly zonal stratospheric winds from tropical radiosonde data (mainly Singapore), Zenodo [data set], https://doi.org/10.5281/zenodo.14037052, 2024.
Laskar, F. I., Chau, J. L., Stober, G., Hoffmann, P., Hall, C. M., and Tsutsumi, M.: Quasi-biennial oscillation modulation of the middle-and high-latitude mesospheric semidiurnal tides during August–September, J. Geophys. Res. Space Phys., 121, 4869–4879, https://doi.org/10.1002/2015JA022065, 2016.
Li, G., Zhao, X., Hu, L., and Xie, H.: Mohe upper atmospheric winds field data, National Earth System Science Data Center, WDC for Geophysics, Beijing [data set], https://doi.org/10.12197/2020ST301, 2020a.
Li, G., Zhao, X., Hu, L., and Xie, H.: Beijing upper atmospheric winds field data, National Earth System Science Data Center, WDC for Geophysics, Beijing [data set], https://doi.org/10.12197/2020ST302, 2020b.
Li, G., Zhao, X., Hu, L., and Xie, H.: Wuhan upper atmospheric winds field data, National Earth System Science Data Center, WDC for Geophysics, Beijing [data set], https://doi.org/10.12197/2020ST303, 2020c.
Li, H., Zhang, J., Sheng, B., Fan, Y., Ji, X., and Li, Q.: The Gravity Wave Activity during Two Recent QBO Disruptions Revealed by U.S. High-Resolution Radiosonde Data, Remote Sens., 15, 472, https://doi.org/10.3390/rs15020472, 2023.
Li, T., She, C. Y., Liu, H., Yue, J., Nakamura, T., and Krueger, D. A.: Observation of local tidal variability and instability, along with dissipation of diurnal tidal harmonics in the mesopause region over Fort Collins, Colorado (41° N, 105° W) (1984–2012), J. Geophys. Res.-Atmos., 114, D06106, https://doi.org/10.1029/2008jd011089, 2009.
Lieberman, R. S.: Long-term variations of zonal mean winds and (1,1) driving in the equatorial lower thermosphere, J. Atmos. Solar-Terrest. Phys., 59, 1483–1490, https://doi.org/10.1016/S1364-6826(96)00150-2, 1997.
Lieberman, R. S., Oberheide, J., Hagan, M. E., Remsberg, E. E., and Gordley, L. L.: Variability of diurnal tides and planetary waves during November 1978–May 1979, J. Atmos. Solar-Terrest. Phys., 66, 517–528, https://doi.org/10.1016/j.jastp.2004.01.006, 2004.
Lieberman, R. S., Riggin, D. M., Ortland, D. A., Nesbitt, S. W., and Vincent, R. A.: Variability of mesospheric diurnal tides and tropospheric diurnal heating during 1997–1998, J. Geophys. Res.-Atmos., 112, D20110, https://doi.org/10.1029/2007jd008578, 2007.
Lindzen, R. S. and Holton, J. R.: A theory of the quasi-biennial oscillation, J. Atmos. Sci., 25, 1095–1107, https://doi.org/10.1175/1520-0469(1968)025<1095:atotqb>2.0.co;2, 1968.
Liu, A. Z., Lu, X., and Franke, S. J.: Diurnal variation of gravity wave momentum flux and its forcing on the diurnal tide, J. Geophys. Res.-Atmos., 118, 1668–1678, https://doi.org/10.1029/2012JD018653, 2013.
Liu, H. L. and Hagan, M. E.: Local heating/cooling of the mesosphere due to gravity wave and tidal coupling, Geophys. Res. Lett., 25, 2941–2944, https://doi.org/10.1029/98GL02153, 1998.
Liu, H.-L., Marsh D. R., She C.-Y., Wu Q., and Xu J.: Momentum balance and gravity wave forcing in the mesosphere and lower thermosphere, Geophys. Res. Lett., 36, L07805, https://doi.org/10.1029/2009GL037252, 2009.
Lu, X., Liu, A. Z., Swenson, G. R., Li, T., Leblanc, T., and McDermid, I. S.: Gravity wave propagation and dissipation from the stratosphere to the lower thermosphere, J. Geophys. Res.-Atmos., 114, D11101, https://doi.org/10.1029/2008JD010112, 2009.
Mayr, H. G. and Mengel, J. G.: Interannual variations of the diurnal tide in the mesosphere generated by the quasi-biennial oscillation, J. Geophys. Res., 110, D10111, https://doi.org/10.1029/2004JD005055, 2005.
McLandress, C.: The seasonal variation of the propagating diurnal tide in the mesosphere and lower thermosphere. Part I: The role of gravity waves and planetary waves, J. Atmos. Sci., 59, 893–906, https://doi.org/10.1175/1520-0469(2002)059<0893:TSVOTP>2.0.CO;2, 2002.
Neale, R. B., Richter, J., Park, S., Lauritzen, P., Vavrus, S., Rasch, P., and Zhang, M.: The mean climate of the Community Atmosphere Model (CAM4) in forced SST and fully coupled experiments, J. Climate, 26, https://doi.org/10.1175/JCLI-D-12-00236.1, 2013.
Newman, P. A., Coy, L., Pawson, S., and Lait, L. R.: The anomalous change in the QBO in 2015–2016, Geophys. Res. Lett., 43, 8791–8797, https://doi.org/10.1002/2016GL070373, 2016.
Ortland, D. A.: Daily estimates of the migrating tide and zonal mean temperature in the mesosphere and lower thermosphere derived from SABER data, J. Geophys. Res.-Atmos., 122, 3754–3785, https://doi.org/10.1002/2016JD025573, 2017.
Osprey, S. M., Butchart, N., Knight, J. R., Scaife, A. A., Hamilton, K., Anstey, J. A., Schenzinger, V., and Zhang, C.: An unexpected disruption of the atmospheric quasi-biennial oscillation, Science, 353, 1424–1427, https://doi.org/10.1126/science.aah4156, 2016.
Pancheva, D., Mukhtarov, P., Hall, C., Meek, C., Tsutsumi, M., Pedatella, N., Nozawa, S., and Manson, A.: Climatology of the main (24-h and 12-h) tides observed by meteor radars at Svalbard and Tromsø: Comparison with the models CMAM-DAS and WACCM-X, J. Atmos. Sol.-Terr. Phy., 207, 105339, https://doi.org/10.1016/j.jastp.2011.04.018, 2020.
Park, M., Randel, W. J., Kinnison, D. E., Bourassa, A. E., Degenstein, D. A., Roth, C. Z., McLinden, C. A., Sioris, C. E., Livesey, N. J., and Santee, M. L.: Variability of stratospheric reactive nitrogen and ozone related to the QBO, J. Geophys. Res.-Atmos., 122, 103–110, 118, https://doi.org/10.1002/2017JD027061, 2017.
Plumb, R. A. and McEwan, A. D.: The instability of a forced standing wave in a viscous stratified fluid: A laboratory analogue of the quasi-biennial oscillation, J. Atmos. Sci., 35, 1827–1839, https://doi.org/10.1175/1520-0469(1978)035<1827:tioafs>2.0.co;2, 1978.
Pramitha, M., Kishore Kumar, K., Venkat Ratnam, M., Praveen, M., and Rao, S. V. B.: Disrupted Stratospheric QBO Signatures in the Diurnal Tides Over the Low-Latitude MLT Region, Geophys. Res. Lett., 48, e2021GL093022, https://doi.org/10.1029/2021GL093022, 2021.
Reed, R. J., Campbell, W. J., Rasmussen, L. A., and Rogers, D. G.: Evidence of a downward- propagating, annual wind reversal in the equatorial stratosphere, J. Geophys. Res., 66, 813–818, https://doi.org/10.1029/JZ066i003p00813, 1961.
Reid, I. M., Spargo, A. J., and Woithe, J. M.: Seasonal variations of the nighttime O(1S) and OH(8-3) airglow intensity at Adelaide, Australia, J. Geophys. Res.-Atmos., 119, 6991–7013, https://doi.org/10.1002/2013JD020906, 2014.
Salinas, C. C. J. H., Wu, D. L., Lee, J. N., Chang, L. C., Qian, L., and Liu, H.: 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, Atmos. Chem. Phys., 23, 1705–1730, https://doi.org/10.5194/acp-23-1705-2023, 2023.
Salawitch, R. J., Weisenstein, D. K., Kovalenko, L. J., Sioris, C. E., Wennberg, P. O., Chance, K., Ko, M. K. W., and McLinden, C. A.: Sensitivity of ozone to bromine in the lower stratosphere, Geophys. Res. Lett., 32, L05811, https://doi.org/10.1029/2004GL021504, 2005.
Sato, K., Watanabe, S., Kawatani, Y., Tomikawa, Y., Miyazaki, K., and Takahashi M.: On the origins of mesospheric gravity waves, Geophys. Res. Lett., 36, L19801, https://doi.org/10.1029/2009GL039908, 2009.
Stober, G., Kuchar, A., Pokhotelov, D., Liu, H., Liu, H.-L., Schmidt, H., Jacobi, C., Baumgarten, K., Brown, P., Janches, D., Murphy, D., Kozlovsky, A., Lester, M., Belova, E., Kero, J., and Mitchell, N.: Interhemispheric differences of mesosphere–lower thermosphere winds and tides investigated from three whole-atmosphere models and meteor radar observations, Atmos. Chem. Phys., 21, 13855–13902, https://doi.org/10.5194/acp-21-13855-2021, 2021.
Stober, G., Liu, A., Kozlovsky, A., Qiao, Z., Krochin, W., Shi, G., Kero, J., Tsutsumi, M., Gulbrandsen, N., Nozawa, S., Lester, M., Baumgarten, K., Belova, E., and Mitchell, N.: Identifying gravity waves launched by the Hunga Tonga–Hunga Ha′apai volcanic eruption in mesosphere/lower-thermosphere winds derived from CONDOR and the Nordic Meteor Radar Cluster, Ann. Geophys., 41, 197–208, https://doi.org/10.5194/angeo-41-197-2023, 2023.
Stober, G., Vadas, S. L., Becker, E., Liu, A., Kozlovsky, A., Janches, D., Qiao, Z., Krochin, W., Shi, G., Yi, W., Zeng, J., Brown, P., Vida, D., Hindley, N., Jacobi, C., Murphy, D., Buriti, R., Andrioli, V., Batista, P., Marino, J., Palo, S., Thorsen, D., Tsutsumi, M., Gulbrandsen, N., Nozawa, S., Lester, M., Baumgarten, K., Kero, J., Belova, E., Mitchell, N., Moffat-Griffin, T., and Li, N.: Gravity waves generated by the Hunga Tonga–Hunga Ha′apai volcanic eruption and their global propagation in the mesosphere/lower thermosphere observed by meteor radars and modeled with the High-Altitude general Mechanistic Circulation Model, Atmos. Chem. Phys., 24, 4851–4873, https://doi.org/10.5194/acp-24-4851-2024, 2024.
Sun, R., Gu, S., Dou, X., and Li, N.: Tidal Structures in the Mesosphere and Lower Thermosphere and Their Solar Cycle Variations, Atmosphere, 13, 2036, https://doi.org/10.3390/atmos13122036, 2022.
University of Science and Technology of China: Atmospheric wind in the MLT region of Mengcheng Meteor Radar, National Space Science Data Center [data set], https://doi.org/10.12176/01.05.021, 2020.
Vichare, G. and Rajaram, R.: Diurnal and semi-diurnal tidal structures due to O2, O3 and H2O heating, J. Earth Syst. Sci., 122, 1207–1217, https://doi.org/10.1007/s12040-013-0353-4, 2013.
Vincent, R. A., Kovalam, S., Fritts, D. C., and Isler, J. R.: Long-term MF radar observations of solar tides in the low-latitude mesosphere: Interannual variability and comparisons with GSWM, J. Geophys. Res., 103, 8667–8683, https://doi.org/10.1029/98JD00482, 1998.
Walterscheid, R. L.: Dynamical cooling induced by dissipating internal gravity waves, Geophys. Res. Lett., 8, 1235–1238, https://doi.org/10.1029/GL008i012p01235, 1981.
Wang, J., Li, N., and Ding, Z.: Zonal and meridional wind tides measured by Kunming meteor radar, Zenodo [data set], https://doi.org/10.5281/zenodo.10829069, 2024.
Yang, C., Smith, A. K., Li, T., and Dou, X.: The effect of the Madden-Julian oscillation on the mesospheric migrating diurnal tide: A study using SDWACCM, Geophys. Res. Lett., 45, 5105–5114, https://doi.org/10.1029/2018GL077956, 2018.
Yulaeva, E. and Wallace, J. M.: The signature of ENSO in global temperature and precipitation fields derived from the microwave sounding unit, J. Climate, 7, 1719–1736, https://doi.org/10.1175/1520-0442(1994)007<1719:TSOEIG>2.0.CO;2, 1994.
Zhang, C. and Zhang, B.: QBO-MJO connection, J. Geophys. Res.-Atmos., 123, 2957–2967, https://doi.org/10.1002/2017JD028171, 2018.
Short summary
We present the impact of quasi-biennial oscillation (QBO) disruption events on diurnal tides over the low- and mid-latitude MLT region observed by a meteor radar chain. By using a global atmospheric model and reanalysis data, it is found that the stratospheric QBO winds can affect the mesospheric diurnal tides by modulating the subtropical ozone variability in the upper stratosphere and the interaction between tides and gravity waves in the mesosphere.
We present the impact of quasi-biennial oscillation (QBO) disruption events on diurnal tides...
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