Articles | Volume 9, issue 10
https://doi.org/10.5194/amt-9-5213-2016
https://doi.org/10.5194/amt-9-5213-2016
Research article
 | 
26 Oct 2016
Research article |  | 26 Oct 2016

A comparison of very short lived halocarbon (VSLS) and DMS aircraft measurements in the tropical west Pacific from CAST, ATTREX and CONTRAST

Stephen J. Andrews, Lucy J. Carpenter, Eric C. Apel, Elliot Atlas, Valeria Donets, James R. Hopkins, Rebecca S. Hornbrook, Alastair C. Lewis, Richard T. Lidster, Richard Lueb, Jamie Minaeian, Maria Navarro, Shalini Punjabi, Daniel Riemer, and Sue Schauffler

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Cited articles

Andreae, M. O.: The Role of Air-Sea Exchange in Geochemical Cycling, chap. The Ocean as a Source of Atmospheric Sulfur Compounds, Springer Netherlands, Dordrecht, 331–362, https://doi.org/10.1007/978-94-009-4738-2_14, 1986.
Andrews, S. J., Hackenberg, S. C., and Carpenter, L. J.: Technical Note: A fully automated purge and trap GC-MS system for quantification of volatile organic compound (VOC) fluxes between the ocean and atmosphere, Ocean Sci., 11, 313–321, https://doi.org/10.5194/os-11-313-2015, 2015.
Andrews, S. J.: Short-lived halocarbon species in the Oceans and Atmosphere, PhD thesis, The University of York, http://etheses.whiterose.ac.uk/id/eprint/5675, 2013.
Andrews, S. J., Jones, C. E., and Carpenter, L. J.: Aircraft measurements of very short-lived halocarbons over the tropical Atlantic Ocean, Geophys. Res. Lett., 40, 1005–1010, 2013.
Apel, E., Hills, A., Lueb, R., Zindel, S., Eisele, S., and Riemer, D.: A fast-GC/MS system to measure C2 to C4 carbonyls and methanol aboard aircraft, J. Geophys. Res.-Atmos., 108, 8794, https://doi.org/10.1029/2002JD003199, 2003.
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We present a comparison of aircraft measurements of important trace gases from a co-ordinated campaign in Jan–Feb 2014 in the tropical west Pacific involving the NASA Global Hawk, NCAR GV and FAAM BAe-146 aircraft. The paper studies the comparability of separate measurements across platforms and demonstrates that aircraft measurements are relevant for characterising the vertical uplift of important gases, such as those with ozone-depleting potential, to the upper troposphere–lower stratosphere.