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

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2012
E. Schweizerbart Science Publishers Stuttgart

Meteorologische Zeitschrift 21, 239 - 244 () [10.1127/0941-2948/2012/0314]

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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.

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Note: We thank the ECMWF for providing the reanalysis data, COST for funding a Short Term Scientific Mission for F. PLOEGER, and in particular N. THOMAS for programming support.

Contributing Institute(s):
  1. Stratosphäre (IEK-7)
Research Program(s):
  1. Atmosphäre und Klima (P23)

Appears in the scientific report 2012
Database coverage:
JCR ; SCOPUS ; Science Citation Index Expanded ; Thomson Reuters Master Journal List ; Web of Science Core Collection ; Zoological Record
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 Record created 2012-11-13, last modified 2024-07-09



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