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''

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Global Change: Climate Variability (1635, 3305, 3309, 4215, 4513), Atmospheric Composition And Structure: Aerosols And Particles (0345, 4801, 4906), Computational Geophysics: Modeling (4255), Cryosphere: Ice Cores (4932), Global Change: Global Climate Models (3337, 4928)

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http://www.agu.org

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