Atmos. Chem. Phys. Discuss., 7, 13989-14010, 2007
www.atmos-chem-phys-discuss.net/7/13989/2007/
doi:10.5194/acpd-7-13989-2007
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Long-term climatology of air mass transport through the Tropical Tropopause Layer (TTL) during NH winter
K. Krüger1,3, S. Tegtmeier2,3, and M. Rex3
1IFM-GEOMAR, Kiel, Germany
2University of Toronto, Toronto, Canada
3Alfred Wegener Institute for Polar and Marine Research, Potsdam, Germany

Abstract. A long-term climatology of air mass transport through the tropical tropopause layer (TTL) is presented, covering the period from 1962–2005. The transport through the TTL is calculated with a Lagrangian approach using radiative heating rates as vertical velocities in an isentropic trajectory model. We demonstrate the improved performance of such an approach compared to previous studies using vertical winds from meteorological analyses. Within the TTL, the averaged diabatic ascent is 0.5 K/day during Northern Hemisphere (NH) winters 1992–2001, close to observations from the tape recorder. Climatological maps show a cooling and strengthening of this part of the residual circulation during the late 1990s and early 2000s compared to the long-term mean. Lagrangian cold point (LCP) fields show systematic differences for varying time periods and natural forcing components. The interannual variability of LCP temperature and density fields are found to be influenced by volcanic eruptions, ENSO, QBO and the solar cycle. The coldest and driest TTL is reached during QBOE and La Niña over the western Pacific, whereas during volcanic eruptions, El Niño and QBOW it is warmer and less dry.

Citation: Krüger, K., Tegtmeier, S., and Rex, M.: Long-term climatology of air mass transport through the Tropical Tropopause Layer (TTL) during NH winter, Atmos. Chem. Phys. Discuss., 7, 13989-14010, doi:10.5194/acpd-7-13989-2007, 2007.
 
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