EGU24-13104, updated on 09 Mar 2024
https://doi.org/10.5194/egusphere-egu24-13104
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Detecting multi-decadal changes in the Brewer-Dobson circulation from in situ trace gas measurements and idealized modeling

Eric Ray1,2, Fred Moore1,3, Brad Hall3, Eric Hintsa1,3, Geoff Dutton1,3, and Hella Garny4
Eric Ray et al.
  • 1CIRES, University of Colorado, Boulder, United States of America (eric.ray@noaa.gov)
  • 2NOAA Chemical Sciences Laboratory
  • 3NOAA Global Monitoring Laboratory
  • 4Institute of Atmospheric Physics, DLR

We utilize in situ stratospheric measurements of trace gases from two recent high altitude aircraft campaigns, DCOTTS and SABRE, to compare mean ages and long-lived trace gas relationships in the NH stratosphere to those from ER-2 campaigns in the 1990s.  The ER-2 campaign data from three decades ago have been a primary reference for in situ-based estimates of mean age in the lower stratosphere from 16-22 km altitude, but very few measurements have been made in this region since then.  We use an updated technique to consistently calculate mean ages from simultaneous in situ measurements of SF6, CO2, N2O and CH4, allowing us to compare mean ages and their relationship with N2O between the 1990s and 2020s.  The mesospheric loss of SF6 and subsequent old age biases are largely accounted for based on newly developed theory and modeling work.  We then use the idealized tropical leaky pipe model to explore stratospheric circulation and mixing changes that are consistent with the observations.

How to cite: Ray, E., Moore, F., Hall, B., Hintsa, E., Dutton, G., and Garny, H.: Detecting multi-decadal changes in the Brewer-Dobson circulation from in situ trace gas measurements and idealized modeling, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-13104, https://doi.org/10.5194/egusphere-egu24-13104, 2024.