(Q58383861)

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Aerosol radiative forcing and climate sensitivity deduced from the Last Glacial Maximum to Holocene transition

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Aerosol radiative forcing and climate sensitivity deduced from the Last Glacial Maximum to Holocene transition (English)

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Ulrike Lohmann

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Petr Chýlek

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Petr Chylek

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English

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publication date

19 February 2008

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published in

Geophysical Research Letters

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volume

35

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issue

4

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Ratio of the Greenland to global temperature change: Comparison of observations and climate modeling results

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Limits on climate sensitivity derived from recent satellite and surface observations

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Radiative forcing of climate by ice-age atmospheric dust

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The Climate Sensitivity and Its Components Diagnosed from Earth Radiation Budget Data

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Climate forcings in Goddard Institute for Space Studies SI2000 simulations

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The role of dust in climate changes today, at the last glacial maximum and in the future

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Climatic impact of ice-age aerosols

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Deriving global climate sensitivity from palaeoclimate reconstructions

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Dust sources and deposition during the last glacial maximum and current climate: A comparison of model results with paleodata from ice cores and marine sediments

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A climate sensitivity test using a global cloud resolving model under an aqua planet condition

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New estimates of radiative forcing due to well mixed greenhouse gases

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Observational evidence of a change in radiative forcing due to the indirect aerosol effect

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Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

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Heat capacity, time constant, and sensitivity of Earth's climate system

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(Q58383861)

Aerosol radiative forcing and climate sensitivity deduced from the Last Glacial Maximum to Holocene transition

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