We investigate the changes in the stratospheric and tropospheric flow that result from a uniform change in SWV using an atmospheric general circulation model (AGCM). The circulation changes are led by the westerly zonal wind anomalies on the upper-poleward edge of the subtropical jets, which are driven in both hemispheres by the strong radiative cooling in the polar lower stratosphere.
We show that the tropospheric response to a uniform increase in SWV is consistent with a poleward shift in the eddy-driven jets. The surface response is largest in boreal winter in both hemispheres, and is focused in the North Atlantic region in the Northern hemisphere.
We compare the circulation changes that result from a uniform fixed SWV perturbation with those from more realistic anomalies in the AGCM. We assess whether changes in SWV similar to those seen in observations could influence the tropospheric circulation at a detectable level, and thus whether changes in SWV may be important for seasonal-to-decadal forecasting.