Climatic impact of spectrally resolved irradiances during the late Archean as modeled with EMAC-FUB

Details Climatic impact of spectrally resolved irradiances during the late Archean as modeled with EMAC-FUB Climatic impact of spectrally resolved irradiances during the late Archean as modeled with EMAC-FUB

Oct 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011epsc.conf.1806k&link_type=abstract

EPSC-DPS Joint Meeting 2011, held 2-7 October 2011 in Nantes, France. http://meetings.copernicus.org/epsc-dps2011, p.1806

Physics

Scientific paper

Investigating the faint young Sun problem we have performed simulations with a 3-dimensional general circulation model. We can show that in an anoxic environment with irradiances valid for the Archaean at 2.5 Ga (i.e. 82% present TSI), a global ocean, and present day greenhouse gases, it is still possible to have liquid water in tropical latitudes, even though the global, annual mean surface temperature is below the freezing point of water.

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