Open AccessGlobal patterns of biomass burning during the last glacial period
Author(s) -
AnneLaure Daniau
Publication year - 2010
Publication title -
pages news
Language(s) - English
Resource type - Journals
eISSN - 1811-1610
pISSN - 1811-1602
DOI - 10.22498/pages.18.2.61
Subject(s) - period (music) , glacial period , biomass burning , physical geography , climatology , geology , biomass (ecology) , environmental science , geography , meteorology , oceanography , paleontology , aerosol , physics , acoustics
Figure 2: Changes in Na (orange) and oxalate concentration (green; ng g) averaged from 68 central Greenland snow-pit samples, from the surface (June 1995) to 2.7 m (1991). Peaks in Na are associated with boreal winters as increased cyclogenesis in the North Atlantic deposits greater concentrations of sea salts on the Greenland Ice Sheet. Orange bars indicate the position of spring snow accumulation. Figure modified from Barbante et al., 2003.
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