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

Viewed

Total article views: 2,476 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,874 535 67 2,476 177 50 59
  • HTML: 1,874
  • PDF: 535
  • XML: 67
  • Total: 2,476
  • Supplement: 177
  • BibTeX: 50
  • EndNote: 59
Views and downloads (calculated since 25 Nov 2021)
Cumulative views and downloads (calculated since 25 Nov 2021)

Viewed (geographical distribution)

Total article views: 2,476 (including HTML, PDF, and XML) Thereof 2,476 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 23 Apr 2025
Download
Short summary
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.
Read more
Share
Altmetrics
Final-revised paper
Preprint