EGU24-2529, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-2529
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Consistent inter-model spread of extratropical westerly jet meridional positions in CMIP6 models between the northern and southern hemispheres in boreal winter

Li Tang1,2, Riyu Lu1,2, and Zhongda Lin1,2
Li Tang et al.
  • 1State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
  • 2University of the Chinese Academy of Sciences, Beijing 100049, China

This study investigates the inter-model spread of extratropical westerly jets between 52 Coupled Model Intercomparison Project phase 6 (CMIP6) models in boreal winter. The results show that there is a substantial spread in latitude of upper-tropospheric westerly jet between models, characterized by large inter-model standard deviations to the poleward and equatorward of jet axis, although the multi-model ensemble mean (MME) of the models performs well in simulating meridional position of westerly jets. Furthermore, we detect the consistency of inter-model jet position spread between the northern and southern hemispheres, based on the inter-model empirical orthogonal function (EOF) decomposition and correlation of regional-averaged zonal winds. Specifically, the models that simulate the westerly jets poleward/equatorward than MME position in one hemisphere tend to also simulate the jets poleward/equatorward in the other hemisphere. Accordingly, we define a global jet spread index to depict the concurrence of jet shift in the two hemispheres. The results of regression analyses based on this index indicate that the models positioning the jets poleward than MME tend to simulate a wider Hadley Cell, a poleward-shifted Ferrel Cell in the southern hemisphere, and a wider intertropical convergence zone (ITCZ). Finally, the inter-model spread of ITCZ width is mainly determined by the spread of convective precipitations between the models, implying that different convection parameterization schemes may play a crucial role in inducing the inter-model spread of extratropical westerly jets and the concurrence of meridional jet shift in the two hemispheres.

How to cite: Tang, L., Lu, R., and Lin, Z.: Consistent inter-model spread of extratropical westerly jet meridional positions in CMIP6 models between the northern and southern hemispheres in boreal winter, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-2529, https://doi.org/10.5194/egusphere-egu24-2529, 2024.