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The upwelling planetary wave activity (PW) from the troposphere controls the intensity of the equator to pole transport of stratospheric ozone by the Brewer-Dobson circulation and thereby modulates the total ozone content at mid-and high-latitudes. Rayleigh lidar temperature data obtained from 1981 to 2001 at mid-latitude were used to study 5doi:10.5194/acpd-6-11299-2006 fatcat:yx4ygce37zhvre7lrrazhxeiz4