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Relative contributions of tropospheric and stratospheric sources to nitrate in Antarctic snow Cover

Relative contributions of tropospheric and stratospheric sources to nitrate in Antarctic snow

Open Access
|Jan 1986

Abstract

The nitrate contents of nearly 500 firn samples collected at various sites on the Antarctic ice sheet are reported. Additional chemical measurements of all major ions, in particular protons, have also been performed so that new conclusions regarding the most probable form and origin of nitrate in the Antarctic can now be drawn.

It is shown that nitrate is deposited as gaseous HNO3 and that tropospheric sources dominate in this remote region. Continental and anthropogenic nitrates are not significant contributors. It is suggested that lightning at tropical and/or mid latitudes is the most likely source of Antarctic nitrate. The formation of HNO3 (or its precursors) in the stratosphere is discussed and the possible evidence for this contribution in several profiles is carefully investigated. The absence of a convincing correlation between solar factors and nitrate concentrations in snow confirms that past solar activity fluctuations cannot be reconstructed from polar ice cores. The spatial and temporal variations observed in this study are, however, not fully explained. Finally, emphasis is placed on the necessity of undertaking HNO3 measurements in the Antarctic atmosphere in order to elucidate the deposition mechanism of this major component of atmospheric chemistry.

Language: English
Page range: 236 - 249
Submitted on: Mar 19, 1986
Accepted on: Apr 30, 1986
Published on: Jan 1, 1986
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 1986 Michel R. Legrand, Robert J. Delmas, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.