Mean age from observations in the lowermost stratosphere: an improved method and interhemispheric differences
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Published:2023-04-03
Issue:7
Volume:23
Page:3887-3903
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Wagenhäuser ThomasORCID, Jesswein MarkusORCID, Keber Timo, Schuck TanjaORCID, Engel AndreasORCID
Abstract
Abstract. The age of stratospheric air is a concept commonly used to
evaluate transport timescales in atmospheric models. The mean age can be
derived from observations of a single long-lived trace gas species with a
known tropospheric trend. Commonly, deriving mean age is based on the
assumption that all air enters the stratosphere through the tropical (TR)
tropopause. However, in the lowermost stratosphere (LMS) close to the
extra-tropical (exTR) tropopause, cross-tropopause transport needs to be
taken into account. We introduce the new exTR–TR method, which considers
exTR input into the stratosphere in addition to TR input. We apply the
exTR–TR method to in situ SF6 measurements from three aircraft
campaigns (PGS, WISE and SouthTRAC) and compare results to those from the
conventional TR-only method. Using the TR-only method, negative mean age
values are derived in the LMS close to the tropopause during the WISE
campaign in Northern Hemispheric (NH) fall 2017. Using the new exTR–TR
method instead, the number and extent of negative mean age values is
reduced. With our new exTR–TR method, we are thus able to derive more
realistic values of typical transport times in the LMS from in situ SF6 measurements. Absolute differences between both methods range from 0.3 to 0.4 years among the three campaigns. Interhemispheric differences in mean age are found when comparing seasonally overlapping campaign phases from the PGS and the SouthTRAC campaigns. On average, within the lowest 65 K potential temperature above the tropopause, the NH LMS is 0.5±0.3 years older around March 2016 than the Southern Hemispheric (SH) LMS
around September 2019. The derived differences between results from the
exTR–TR method and the TR-only method, as well as interhemispheric
differences, are higher than the sensitivities of the exTR–TR method to
parameter uncertainties, which are estimated to be below 0.22 years for all
three campaigns.
Funder
Deutsche Forschungsgemeinschaft National Aeronautics and Space Administration
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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