Climatology of pure tropospheric profiles and column contents of ozone and carbon monoxide using MOZAIC in the mid-northern latitudes (24° N to 50° N) from 1994 to 2009

Abstract

The objective of this paper is to deliver the most accurate ozone (O 3) and carbon monoxide (CO) climatology for the pure troposphere only, i.e. exclusively from the ground to the dynamical tropopause on an individual profile basis. The results (profiles and columns) are derived solely from the Measurements of OZone and water vapour by in-service AIrbus airCraft programme (MOZAIC) over 15 years (1994-2009). The study, focused on the northern midlatitudes [24-50° N] and [119°W-140° E], includes more than 40 000 profiles over 11 sites to give a quasi-global zonal picture. Considering all the sites, the pure tropospheric column peak-to-peak seasonal cycle ranges are 23.7-43.2DU for O3 and 1.7-6.9×1018 molecules cm-2 for CO. The maxima of the seasonal cycles are not in phase, occurring in February-April for CO and May-July for O3. The phase shift is related to the photochemistry and OH removal efficiencies. The purely tropospheric seasonal profiles are characterized by a typical autumn-winter/spring-summer O3 dichotomy (except in Los Angeles, Eastmed - a cluster of Cairo and Tel Aviv - and the regions impacted by the summer monsoon) and a summer-autumn/winter-spring CO dichotomy. We revisit the boundary-layer, mid-tropospheric (MT) and uppertropospheric (UT) partial columns using a new monthly varying MT ceiling. Interestingly, the seasonal cycle maximum of the UT partial columns is shifted from summer to spring for O 3 and to very early spring for CO. Conversely, the MT maximum is shifted from spring to summer and is associated with a summer (winter) MT thickening (thinning). Lastly, the pure tropospheric seasonal cycles derived from our analysis are consistent with the cycles derived from spaceborne measurements, the correlation coefficients being r = 0.6-0.9 for O3 and r > 0.9 for CO. The cycles observed from space are nevertheless greater than MOZAIC for O3 (by 9-18 DU) and smaller for CO (up to 1×1018 molecules cm-2). The larger winter O 3 difference between the two data sets suggests probable stratospheric contamination in satellite data due to the tropopause position. The study underlines the importance of rigorously discriminating between the stratospheric and tropospheric reservoirs and avoiding use of a monthly averaged tropopause position without this strict discrimination in order to assess the pure O3 and CO tropospheric trends. © Author(s) 2013.