Backtrajectory reconstruction of water vapour and ozone in-situ observations in the TTL

Author: Ploeger F.   Konopka P.   Müller R.   Günther G.   Grooss J.-U.   Schiller C.   Ravegnani F.   Ulanovski A.   Riese M.  

Publisher: E. Schweizerbart'sche Verlagsbuchhandlung

ISSN: 0941-2948

Source: Meteorologische Zeitschrift, Vol.21, Iss.3, 2012-06, pp. : 239-244

Disclaimer: Any content in publications that violate the sovereignty, the constitution or regulations of the PRC is not accepted or approved by CNPIEC.

Previous Menu Next

Abstract

Water vapour and ozone in-situ observations in the tropical tropopause layer (TTL) during the three tropical campaigns SCOUT-O3, AMMA and TroCCiNOx are reconstructed from diabatic and kinematic backtrajectories, with the reconstruction method for the tracer fields based on freeze-drying and photochemichal ozone production. The results using diabatic trajectories show that both water vapour and ozone in-situ observations can be well reconstructed from trajectories. Consequentially, in-situ observations agree with the assumption of freeze-drying due to the large-scale temperature field as the main control mechanism for water vapour and photochemical production and transport as main control mechanisms for tropical ozone. The kinematic ozone reconstruction, however, shows a large high-bias during SCOUT-O3 and a too strong variability during all campaigns, due to excessive transport of stratospheric ozone into the TTL. We conclude that kinematic reconstructions of in-situ observations are less reliable than diabatic, due to unrealistic inhomogeneities in the velocity field.

Related content