The stratosphere is the middle layer of the atmosphere, and the home of the ozone layer, which protects the Earth from harmful ultraviolet radiation. Recent long-term changes in many stratospheric trace gases, including ozone, have opposite signs in the Southern Hemisphere (SH) compared to the Northern Hemisphere (NH). This is at least partly due to hemispherically asymmetric changes in the transport rate within the stratosphere, but changes in the transport rate are difficult to quantify as it cannot be directly measured. We used satellite observations and model simulations of trace gases to show that since 2004 the transport rate in the NH has been slower than the transport rate in the SH. This is important to consider when evaluating the recovery of the ozone layer.