Nature Communications (Jan 2016)

A pervasive role for biomass burning in tropical high ozone/low water structures

  • Daniel C. Anderson,
  • Julie M. Nicely,
  • Ross J. Salawitch,
  • Timothy P. Canty,
  • Russell R. Dickerson,
  • Thomas F. Hanisco,
  • Glenn M. Wolfe,
  • Eric C. Apel,
  • Elliot Atlas,
  • Thomas Bannan,
  • Stephane Bauguitte,
  • Nicola J. Blake,
  • James F. Bresch,
  • Teresa L. Campos,
  • Lucy J. Carpenter,
  • Mark D. Cohen,
  • Mathew Evans,
  • Rafael P. Fernandez,
  • Brian H. Kahn,
  • Douglas E. Kinnison,
  • Samuel R. Hall,
  • Neil R.P. Harris,
  • Rebecca S. Hornbrook,
  • Jean-Francois Lamarque,
  • Michael Le Breton,
  • James D. Lee,
  • Carl Percival,
  • Leonhard Pfister,
  • R. Bradley Pierce,
  • Daniel D. Riemer,
  • Alfonso Saiz-Lopez,
  • Barbara J.B. Stunder,
  • Anne M. Thompson,
  • Kirk Ullmann,
  • Adam Vaughan,
  • Andrew J. Weinheimer

DOI
https://doi.org/10.1038/ncomms10267
Journal volume & issue
Vol. 7, no. 1
pp. 1 – 13

Abstract

Read online

High ozone and low water structures in the tropical western Pacific are commonly attributed to transport from the stratosphere or mid-latitudes. Here, Anderson et al. show these structures actually result from ozone production in biomass burning plumes and large-scale descent of air within the tropics.