Articles | Volume 17, issue 6
https://doi.org/10.5194/acp-17-4337-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-4337-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
30 Mar 2017
Research article |
| 30 Mar 2017
Role of vertical and horizontal mixing in the tape recorder signal near the tropical tropopause
Anne A. Glanville
Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA
Thomas Birner
CORRESPONDING AUTHOR
Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA
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Cited
15 citations as recorded by crossref.
- Multitimescale variations in modeled stratospheric water vapor derived from three modern reanalysis products M. Tao et al. 10.5194/acp-19-6509-2019
- Turbulence in the tropical stratosphere, equatorial Kelvin waves, and the quasi-biennial oscillation R. Atlas et al. 10.1073/pnas.2409791122
- Diagnosing Observed Stratospheric Water Vapor Relationships to the Cold Point Tropical Tropopause W. Randel & M. Park 10.1029/2019JD030648
- Coordinated Upper-Troposphere-to-Stratosphere Balloon Experiment in Biak F. Hasebe et al. 10.1175/BAMS-D-16-0289.1
- Quantifying the effect of mixing on the mean age of air in CCMVal-2 and CCMI-1 models S. Dietmüller et al. 10.5194/acp-18-6699-2018
- Upper tropospheric ozone transport from the sub-tropics to tropics over the Indian region during Asian summer monsoon S. Das et al. 10.1007/s00382-018-4418-6
- Climate, Variability, and Climate Sensitivity of “Middle Atmosphere” Chemistry Configurations of the Community Earth System Model Version 2, Whole Atmosphere Community Climate Model Version 6 (CESM2(WACCM6)) N. Davis et al. 10.1029/2022MS003579
- Stratospheric Adiabatic Mixing Rates Derived From the Vertical Gradient of Age of Air M. Linz et al. 10.1029/2021JD035199
- Sensitivities of modelled water vapour in the lower stratosphere: temperature uncertainty, effects of horizontal transport and small-scale mixing L. Poshyvailo et al. 10.5194/acp-18-8505-2018
- On the relative importance of radiative and dynamical heating for tropical tropopause temperatures T. Birner & E. Charlesworth 10.1002/2016JD026445
- Nearly identical cycles of the quasi‐biennial oscillation in the equatorial lower stratosphere T. Dunkerton 10.1002/2017JD026542
- Response of stratospheric water vapor and ozone to the unusual timing of El Niño and the QBO disruption in 2015–2016 M. Diallo et al. 10.5194/acp-18-13055-2018
- Equatorward dispersion of a high-latitude volcanic plume and its relation to the Asian summer monsoon: a case study of the Sarychev eruption in 2009 X. Wu et al. 10.5194/acp-17-13439-2017
- The global diabatic circulation of the stratosphere as a metric for the Brewer–Dobson circulation M. Linz et al. 10.5194/acp-19-5069-2019
- Small-Scale Wind Fluctuations in the Tropical Tropopause Layer from Aircraft Measurements: Occurrence, Nature, and Impact on Vertical Mixing A. Podglajen et al. 10.1175/JAS-D-17-0010.1
15 citations as recorded by crossref.
- Multitimescale variations in modeled stratospheric water vapor derived from three modern reanalysis products M. Tao et al. 10.5194/acp-19-6509-2019
- Turbulence in the tropical stratosphere, equatorial Kelvin waves, and the quasi-biennial oscillation R. Atlas et al. 10.1073/pnas.2409791122
- Diagnosing Observed Stratospheric Water Vapor Relationships to the Cold Point Tropical Tropopause W. Randel & M. Park 10.1029/2019JD030648
- Coordinated Upper-Troposphere-to-Stratosphere Balloon Experiment in Biak F. Hasebe et al. 10.1175/BAMS-D-16-0289.1
- Quantifying the effect of mixing on the mean age of air in CCMVal-2 and CCMI-1 models S. Dietmüller et al. 10.5194/acp-18-6699-2018
- Upper tropospheric ozone transport from the sub-tropics to tropics over the Indian region during Asian summer monsoon S. Das et al. 10.1007/s00382-018-4418-6
- Climate, Variability, and Climate Sensitivity of “Middle Atmosphere” Chemistry Configurations of the Community Earth System Model Version 2, Whole Atmosphere Community Climate Model Version 6 (CESM2(WACCM6)) N. Davis et al. 10.1029/2022MS003579
- Stratospheric Adiabatic Mixing Rates Derived From the Vertical Gradient of Age of Air M. Linz et al. 10.1029/2021JD035199
- Sensitivities of modelled water vapour in the lower stratosphere: temperature uncertainty, effects of horizontal transport and small-scale mixing L. Poshyvailo et al. 10.5194/acp-18-8505-2018
- On the relative importance of radiative and dynamical heating for tropical tropopause temperatures T. Birner & E. Charlesworth 10.1002/2016JD026445
- Nearly identical cycles of the quasi‐biennial oscillation in the equatorial lower stratosphere T. Dunkerton 10.1002/2017JD026542
- Response of stratospheric water vapor and ozone to the unusual timing of El Niño and the QBO disruption in 2015–2016 M. Diallo et al. 10.5194/acp-18-13055-2018
- Equatorward dispersion of a high-latitude volcanic plume and its relation to the Asian summer monsoon: a case study of the Sarychev eruption in 2009 X. Wu et al. 10.5194/acp-17-13439-2017
- The global diabatic circulation of the stratosphere as a metric for the Brewer–Dobson circulation M. Linz et al. 10.5194/acp-19-5069-2019
- Small-Scale Wind Fluctuations in the Tropical Tropopause Layer from Aircraft Measurements: Occurrence, Nature, and Impact on Vertical Mixing A. Podglajen et al. 10.1175/JAS-D-17-0010.1
Latest update: 02 Apr 2025
Short summary
Nearly all air enters the stratosphere through the tropical tropopause, which exerts a control on stratospheric chemistry and climate. By combining satellite observations with a simple 1-D transport model, we study the roles of vertical and horizontal mixing in transport near the tropical tropopause. We find that vertical mixing may play a more significant role than previously assumed, which is potentially as important as slow vertical transport by the residual mass circulation.
Nearly all air enters the stratosphere through the tropical tropopause, which exerts a control...
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