Quantifying sources and sinks of reactive gases in the lower atmosphere using airborne flux observations

G. M. Wolfe, T. F. Hanisco, H. L. Arkinson, T. P. Bui, J. D. Crounse, J. Dean-Day, A. Goldstein, A. Guenther, S. R. Hall, G. Huey, D. J. Jacob, T. Karl, P. S. Kim, X. Liu, M. R. Marvin, T. Mikoviny, P. K. Misztal, T. B. Nguyen, J. Peischl, I. PollackT. Ryerson, J. M. St. Clair, A. Teng, K. R. Travis, K. Ullmann, P. O. Wennberg, A. Wisthaler

Research output: Contribution to journalArticlepeer-review

50 Scopus citations

Abstract

Atmospheric composition is governed by the interplay of emissions, chemistry, deposition, and transport. Substantial questions surround each of these processes, especially in forested environments with strong biogenic emissions. Utilizing aircraft observations acquired over a forest in the southeast U.S., we calculate eddy covariance fluxes for a suite of reactive gases and apply the synergistic information derived from this analysis to quantify emission and deposition fluxes, oxidant concentrations, aerosol uptake coefficients, and other key parameters. Evaluation of results against state-of-the-science models and parameterizations provides insight into our current understanding of this system and frames future observational priorities. As a near-direct measurement of fundamental process rates, airborne fluxes offer a new tool to improve biogenic and anthropogenic emissions inventories, photochemical mechanisms, and deposition parameterizations.

Original languageEnglish
Pages (from-to)8231-8240
Number of pages10
JournalGeophysical Research Letters
Volume42
Issue number19
DOIs
StatePublished - Oct 16 2015
Externally publishedYes

Keywords

  • SEAC4RS
  • biosphere
  • deposition
  • emission
  • flux
  • isoprene

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