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AGU: Geophysical Research Letters

 

Keywords

  • climate sensitivity
  • aerosol radiative forcing
  • Last Glacial Maximum

Index Terms

  • Global Change: Climate variability
  • Atmospheric Composition and Structure: Aerosols and particles
  • Computational Geophysics: Modeling
  • Cryosphere: Ice cores
  • Global Change: Global climate models

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L23704, 3 PP., 2008
doi:10.1029/2008GL034308

Reply to comment by Andrey Ganopolski and Thomas Schneider von Deimling on “Aerosol radiative forcing and climate sensitivity deduced from the Last Glacial Maximum to Holocene transition”

Petr Chylek

Space and Remote Sensing, Los Alamos National Laboratory, Los Alamos, New Mexico, USA

Ulrike Lohmann

Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland

Received 15 April 2008; accepted 23 October 2008; published 5 December 2008.

Citation: Chylek, P., and U. Lohmann (2008), Reply to comment by Andrey Ganopolski and Thomas Schneider von Deimling on “Aerosol radiative forcing and climate sensitivity deduced from the Last Glacial Maximum to Holocene transition”, Geophys. Res. Lett., 35, L23704, doi:10.1029/2008GL034308.

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