Atmos. Chem. Phys., 8, 813-823, 2008
www.atmos-chem-phys.net/8/813/2008/
doi:10.5194/acp-8-813-2008
© Author(s) 2008. This work is distributed
under the Creative Commons Attribution 3.0 License.
Long-term climatology of air mass transport through the Tropical Tropopause Layer (TTL) during NH winter
K. Krüger1,*, S. Tegtmeier1,**, and M. Rex1
1Alfred Wegener Institute for Polar and Marine Research, Potsdam, Germany
*now at: IFM-GEOMAR, Kiel, Germany
**now at: University of Toronto, Toronto, Canada

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 upper part of the TTL, the averaged diabatic ascent is 0.5 K/day during Northern Hemisphere (NH) winters 1992–2001. Climatological maps show a cooling and strengthening of this part of the residual circulation during the 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 is found to be influenced by volcanic eruptions, El Niño Southern Oscillation (ENSO), Quasi-Biennial Oscillation (QBO) and the solar cycle. The coldest and driest TTL is reached during QBO easterly phase and La Niña over the western Pacific, whereas during volcanic eruptions, El Niño and QBO westerly phase 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., 8, 813-823, doi:10.5194/acp-8-813-2008, 2008.
 
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