Factors controlling nitrate in ice cores: Evidence from the Dome C deep ice core

Röthlisberger, Regine; Hutterli, Manuel A.; Sommer, Stefan; Wolff, Eric W.; Mulvaney, Robert ORCID: https://orcid.org/0000-0002-5372-8148. 2000 Factors controlling nitrate in ice cores: Evidence from the Dome C deep ice core. Journal of Geophysical Research, 105 (D16). 20565-20572. https://doi.org/10.1029/2000JD900264

Before downloading, please read NORA policies.

Preview

Text (An edited version of this paper was published by AGU. Copyright American Geophysical Union.) jgrd7630.pdf - Published Version Download (919kB) | Preview

Abstract/Summary

In order to estimate past changes in atmospheric NOx concentration, nitrate, an oxidation product of NOx, has often been measured in polar ice cores. In the frame of the European Project for Ice Coring in Antarctica (EPICA), a high-resolution nitrate record was obtained by continuous flow analysis (CFA) of a new deep ice core drilled at Dome C. This record allows a detailed comparison of nitrate with other chemical trace substances in polar snow under different climatic regimes. Previous studies showed that it would be difficult to make firm conclusions about atmospheric NOx concentrations based on ice core nitrate without a better understanding of the factors controlling NO3− deposition and preservation. At Dome C, initially high nitrate concentrations (over 500 ppb) decrease within the top meter to steady low values around 15 ppb that are maintained throughout the Holocene ice. Much higher concentrations (averaging 53 ppb) are found in ice from the Last Glacial Maximum (LGM). Combining this information with data from previous sampling elsewhere in Antarctica, it seems that under climatic conditions of the Holocene, temperature and accumulation rate are the key factors determining the NO3− concentration in the ice. Furthermore, ice layers with high acidity show a depletion of NO3−, but higher concentrations are found before and after the acidity layer, indicating that NO3− has been redistributed after deposition. Under glacial conditions, where NO3− shows a higher concentration level and also a larger variability, non-sea-salt calcium seems to act as a stabilizer, preventing volatilization of NO3− from the surface snow layers.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1029/2000JD900264
Programmes:	BAS Programmes > Pre 2000 programme
ISSN:	0148-0227
Additional Keywords:	polar ice cores, NOx concentration, Dome C, Antarctica, continuous flow analysis, CFA, European Project for Ice Coring in Antarctica, EPICA
NORA Subject Terms:	Glaciology Atmospheric Sciences Chemistry
Date made live:	08 Jul 2013 09:14 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/502387

Actions (login required)

View Item

Document Downloads

More statistics for this item...