- 1Harvard University, School of Engineering and Applied Sciences, Cambridge MA, United States of America (kirstinkoepnick@g.harvard.edu)
- 2School of the Environment and Earth Sciences, Tel Aviv University, Tel Aviv, Israel (harnik@tauex.tau.ac.il)
- 3Department of Atmospheric Sciences, Colorado State University, Fort Collins CO, United States of America (David.Randall@colostate.edu )
- 4Harvard University, Department of Earth and Planetary Sciences, Cambridge MA, United States of America (eli@eps.harvard.edu)
There is a long history of studies of potential interactions between the El Niño–Southern Oscillation (ENSO) and the quasi-biennial oscillation (QBO). Some suggested that ENSO may modulate QBO phase transitions or amplitude, although identifying a straightforward correlation of the two variability modes has been elusive. Recent studies showed some interesting connections between the surface composites of the two modes, sea surface temperature in particular. However, the observed record is short and noisy, raising the question whether such patterns reflect a robust dynamical coupling or a statistical artifact. In this talk, I will show the observed patterns from ERA5 show and therefore imply. Additionally, I will then discuss how the various high-top CMIP6 models produce (or do not produce) the observed signal. By comparing model output with observations, we assess the extent to which apparent correlations are reproducible by this physical mechanism or can be identified as an artifact.
How to cite: Koepnick, K., Harnik, N., Randall, D., and Tziperman, E.: ENSO-QBO correlations: a robust dynamical coupling or a coincidence due to the short record? , EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-3547, https://doi.org/10.5194/egusphere-egu26-3547, 2026.