Preprints
https://doi.org/10.5194/egusphere-2022-998
https://doi.org/10.5194/egusphere-2022-998
 
13 Oct 2022
13 Oct 2022

Signatures of the Madden-Julian Oscillation in Middle Atmosphere zonal mean Temperature: Triggering the Interhemispheric Coupling pattern

Christoph G. Hoffmann1, Lena G. Buth1,a, and Christian von Savigny1 Christoph G. Hoffmann et al.
  • 1Institute of Physics, University of Greifswald, Felix-Hausdorff-Str. 6, 17489 Greifswald, Germany
  • anow at: Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany

Abstract. The Madden–Julian oscillation (MJO) is the dominant mode of intraseasonal variability in the troposphere. The influence of the MJO on the middle atmosphere (MA) and particularly on its temperature is of interest for both the understanding of MJO-induced teleconnections and research on the variability of the middle atmosphere. However, only few studies dealing with the influence of the MJO on MA temperature are available.

We analyze statistically the connection of the MJO and the MA zonal mean temperature based on observations by the MLS satellite instrument. We consider all eight MJO phases, different seasons and the state of the quasi-biennial oscillation (QBO). We show that the MA temperature is influenced by the state of MJO in large areas of the MA and under roughly all considered atmospheric conditions. The zonal mean temperature response is characterized by a particular spatial pattern, which we link to the interhemispheric coupling (IHC) mechanism, a known dynamical feature of the MA. The strongest temperature deviations are on the order of ± 10 K and are found in the polar winter MA during boreal winter when the QBO is in the easterly phase. Other atmospheric conditions also show temperature responses with the characteristic spatial pattern, but weaker and more noisy. The QBO turns out to have a relatively big influence during boreal winter but only a small influence during austral winter. We also discuss the role of sudden stratospheric warmings (SSWs), which have an ambivalent influence on our interpretation, because they introduce strong temperature variability in the polar winter MA themselves. In addition, SSWs are one possibility to explain the QBO influence during boreal winter. Furthermore, we also analyze the change of the temperature response pattern while the MJO progresses from one phase to the next. We find a largely systematic reaction of the MA to the phase changes, particularly a gradual altitude shift of the MA temperature response pattern, which can be seen more or less clearly depending on the atmospheric conditions.

Overall, a major outcome of the present study is the finding that the tropospheric MJO can trigger the IHC mechanism, which affects many areas of the MA. It is therefore a noteworthy example for the complex couplings across different atmospheric layers and geographical regions in the atmosphere. Additionally, it highlights close linkages of known dynamical features of the atmosphere, particularly the MJO, the IHC, the QBO, and SSWs.

Because of the wide coverage of atmospheric regions and included dynamical features, the results might help to further constrain the underlying dynamical mechanisms and could be used as a benchmark for the representation of atmospheric couplings on the intraseasonal timescale in atmospheric models.

Christoph G. Hoffmann et al.

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on egusphere-2022-998', Paul PUKITE, 16 Oct 2022
    • CC2: 'Reply on CC1', Paul PUKITE, 16 Oct 2022
      • CC3: 'Reply on CC2', Paul PUKITE, 16 Oct 2022
  • RC1: 'Comment on egusphere-2022-998', Anonymous Referee #1, 14 Nov 2022
  • RC2: 'Comment on egusphere-2022-998', Anonymous Referee #2, 15 Nov 2022

Christoph G. Hoffmann et al.

Christoph G. Hoffmann et al.

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Short summary
The Madden–Julian oscillation is an important feature of weather in the Tropics. Although it is mainly active in the troposphere, we show that it systematically influences the air temperature in the layers above – up to about 100 km altitude and from pole to pole. We have linked this to another known far-reaching process, the interhemispheric coupling. This is basic research on atmospheric couplings and variability, but might also be of interest for intraseasonal weather forecasting models.