GCM analysis of local influences on ice core δ signals

Details GCM analysis of local influences on ice core δ signals GCM analysis of local influences on ice core δ signals

Nov 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997georl..24.2825k&link_type=abstract

Geophysical Research Letters, Volume 24, Issue 22, p. 2825-2828

Physics

60

Meteorology And Atmospheric Dynamics: Climatology, Meteorology And Atmospheric Dynamics: General Or Miscellaneous

Scientific paper

A high resolution GCM is used to examine the effect of changes in local surface climate parameters on the ice sheets that can influence the interpretation of the isotopic signal of the ice from deep cores. The model suggests that the 10°C difference between the LGM surface temperature deduced from borehole thermometry and that deduced from the water isotope analysis to a great extent may be due to a modification of the precipitation seasonality in central Greenland. For central East Antarctica, the model tends to suggest a weak opposite bias.

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