Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics
ACP
Articles | Volume 22, issue 12
Articles | Volume 22, issue 12
https://doi.org/10.5194/acp-22-7861-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-22-7861-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 22, issue 12
Research article
 | 
17 Jun 2022
Research article |  | 17 Jun 2022

Suppressed migrating diurnal tides in the mesosphere and lower thermosphere region during El Niño in northern winter and its possible mechanism

Yetao Cen, Chengyun Yang, Tao Li, James M. Russell III, and Xiankang Dou

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Auclair-Desrotour, P., Laskar, J., and Mathis, S.: Atmospheric tides and their consequences on the rotational dynamics of terrestrial planets, EAS Publications, 82, 81–90, https://doi.org/10.1051/eas/1982008, 2017. 
Baumgarten, K., Gerding, M., Baumgarten, G., and Lübken, F.-J.: Temporal variability of tidal and gravity waves during a record long 10-day continuous lidar sounding, Atmos. Chem. Phys., 18, 371–384, https://doi.org/10.5194/acp-18-371-2018, 2018. 
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. 
Calvo-Fernández, N., Herrera, R. G., Puyol, D. G. , Martín, E. H., García, R. R., Presa, L. G., and Rodriguez, P. R.: Analysis of the enso signal in tropospheric and stratospheric temperatures observed by MSU, 1979–2000, J. Climate, 17, 3934–3946, https://doi.org/10.1175/1520-0442(2004)017<3934:aotesi>2.0.co;2, 2004. 
Cen, Y.: 1979–2014 SDWACCM data, figshare [data set], https://doi.org/10.6084/m9.figshare.19777918, 2022. 
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The MLT DW1 amplitude is suppressed during El Niño winters in both satellite observation and SD-WACCM simulations. The suppressed Hough mode (1, 1) in the tropopause region propagates vertically to the MLT region, leading to decreased DW1 amplitude. The latitudinal zonal wind shear anomalies during El Niño winters would narrow the waveguide and prevent the vertical propagation of DW1. The gravity wave drag excited by ENSO-induced anomalous convection could also modulate the MLT DW1 amplitude.
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