Implication of azelaic acid in a Greenland ice core for oceanic and atmospheric changes in high latitudes

Details Implication of azelaic acid in a Greenland ice core for oceanic and atmospheric changes in high latitudes Implication of azelaic acid in a Greenland ice core for oceanic and atmospheric changes in high latitudes

Apr 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999georl..26..871k&link_type=abstract

Geophysical Research Letters, Volume 26, Issue 7, p. 871-874

Mathematics

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Atmospheric Composition And Structure: Biosphere/Atmosphere Interactions, Hydrology: Snow And Ice, Information Related To Geographic Region: Arctic Region, Oceanography: Biological And Chemical: Photochemistry

Scientific paper

A Greenland ice core (450 years) has been studied for low molecular weight dicarboxylic acids (C2-C10) using a capillary gas chromatography and mass spectrometer. Their molecular distribution generally showed a predominance of succinic acid (C4) followed by oxalic (C2), malonic (C3), glutaric (C5), adipic (C6), and azelaic (C9) acids. Azelaic acid, that is a specific photochemical reaction product of biogenic unsaturated fatty acids, gave a characteristic historical trend in the ice core; i.e., the concentrations are relatively low during late 16th to 19th century (Little Ice Age) but become very high in late 19th to 20th century (warmer periods) with a large peak in 1940s AD. Lower concentrations of azelaic acid may have been caused by a depressed emission of unsaturated fatty acids from seawater microlayers due to enhanced sea ice coverage during Little Ice Age. Inversely, increased concentrations of azelaic acid in late 19th to 20th century are likely interpreted by an enhanced sea-to-air emission of the precursor unsaturated fatty acids due to a retreat of sea ice and/or by the enhanced production due to a potentially increased oxidizing capability of the atmosphere.

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