The negative meridional moisture gradient reduces African easterly jet magnitude by 30% through vapor buoyancy counteracting the temperature gradient in thermal wind balance, with the effect strengthening under global warming in CMIP6 data.
Tropical tropospheric warming pattern explained by shifts in convective heating in the
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Water vapor buoyancy and the African easterly jet
The negative meridional moisture gradient reduces African easterly jet magnitude by 30% through vapor buoyancy counteracting the temperature gradient in thermal wind balance, with the effect strengthening under global warming in CMIP6 data.