Nature Communications (Apr 2018)

Greenland records of aerosol source and atmospheric lifetime changes from the Eemian to the Holocene

  • S. Schüpbach,
  • H. Fischer,
  • M. Bigler,
  • T. Erhardt,
  • G. Gfeller,
  • D. Leuenberger,
  • O. Mini,
  • R. Mulvaney,
  • N. J. Abram,
  • L. Fleet,
  • M. M. Frey,
  • E. Thomas,
  • A. Svensson,
  • D. Dahl-Jensen,
  • E. Kettner,
  • H. Kjaer,
  • I. Seierstad,
  • J. P. Steffensen,
  • S. O. Rasmussen,
  • P. Vallelonga,
  • M. Winstrup,
  • A. Wegner,
  • B. Twarloh,
  • K. Wolff,
  • K. Schmidt,
  • K. Goto-Azuma,
  • T. Kuramoto,
  • M. Hirabayashi,
  • J. Uetake,
  • J. Zheng,
  • J. Bourgeois,
  • D. Fisher,
  • D. Zhiheng,
  • C. Xiao,
  • M. Legrand,
  • A. Spolaor,
  • J. Gabrieli,
  • C. Barbante,
  • J.-H. Kang,
  • S. D. Hur,
  • S. B. Hong,
  • H. J. Hwang,
  • S. Hong,
  • M. Hansson,
  • Y. Iizuka,
  • I. Oyabu,
  • R. Muscheler,
  • F. Adolphi,
  • O. Maselli,
  • J. McConnell,
  • E. W. Wolff

DOI
https://doi.org/10.1038/s41467-018-03924-3
Journal volume & issue
Vol. 9, no. 1
pp. 1 – 10

Abstract

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Past climate changes in Greenland ice were accompanied by large aerosol concentration changes. Here, the authors show that by correcting for transport effects, reliable source changes for biogenic aerosol from North America, sea salt aerosol from the North Atlantic, and dust from East Asian deserts can be derived.