Age of air from in situ trace gas measurements: insights from a new technique

Abstract. The age of air is an important transport diagnostic that can be derived from trace gas measurements and compared to global chemistry climate model output. We describe a new technique to calculate the age of air, measuring transport times from the Earth's surface to any location in the atmosphere based on simultaneous in situ measurements of multiple key long-lived trace gases. The primary benefits of this new technique include (1) optimized ages of air consistent with simultaneously measured SF6 and CO2; (2) age of air from the upper troposphere through the stratosphere; (3) estimates of the second moment of age spectra that have not been well constrained from measurements; and (4) flexibility to be used with measurements across multiple instruments, platforms, and decades. We demonstrate the technique on aircraft and balloon measurements from the 1990s, the last period of extensive stratospheric in situ sampling, and several recent missions from the 2020s, and compare the results with previously published and modeled values.

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Publication Details

Journal
Atmospheric chemistry and physics
Published
2024-11-11
DOI
https://doi.org/10.5194/acp-24-12425-2024
Citations
7
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
2.63

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article

Age of air from in situ trace gas measurements: insights from a new technique

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7 citations
Atmospheric chemistry and physics
Atmospheric chemistry and aerosols
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article

Age of air from in situ trace gas measurements: insights from a new technique

David Nance, Colm Sweeney, F. L. Moore, Jianghanyang Li, Eric J. Hintsa, Bianca C. Baier, Eric Ray, B. D. Hall, Hella Garny, James W. Elkins, Steven C. Wofsy, G. S. Dutton, Bruce C. Daube, J. V. Pittman
article en
7 citations

Abstract

Abstract. The age of air is an important transport diagnostic that can be derived from trace gas measurements and compared to global chemistry climate model output. We describe a new technique to calculate the age of air, measuring transport times from the Earth's surface to any location in the atmosphere based on simultaneous in situ measurements of multiple key long-lived trace gases. The primary benefits of this new technique include (1) optimized ages of air consistent with simultaneously measured SF6 and CO2; (2) age of air from the upper troposphere through the stratosphere; (3) estimates of the second moment of age spectra that have not been well constrained from measurements; and (4) flexibility to be used with measurements across multiple instruments, platforms, and decades. We demonstrate the technique on aircraft and balloon measurements from the 1990s, the last period of extensive stratospheric in situ sampling, and several recent missions from the 2020s, and compare the results with previously published and modeled values.

Atmospheric chemistry and physicsVol. 24(21)
Planetary Science Institute (US), Harvard University (US), Cooperative Institute for Research in Environmental Sciences (US), Institute of Arctic and Alpine Research (US), University of Colorado Boulder (US), Deutsches Zentrum für Luft- und Raumfahrt e. V. (DLR) (DE), NOAA Chemical Sciences Laboratory (US), Ludwig-Maximilians-Universität München (DE)
NOAA Research
Climate action
Openalex Percentile: Top 10%
Atmospheric chemistry and aerosols
2.63
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