Climatic implications of background acidity and other chemistry derived from electrical studies of the Greenland Ice Core Project ice core

Wolff, Eric W.; Moore, John C.; Clausen, Henrik B.; Hammer, Claus U.. 1997 Climatic implications of background acidity and other chemistry derived from electrical studies of the Greenland Ice Core Project ice core. Journal of Geophysical Research: Oceans, 102 (C12). 26325-26332. 10.1029/96JC02223

Full text not available from this repository. (Request a copy)

Official URL: http://dx.doi.org/10.1029/96JC02223

Abstract/Summary

High-resolution continuous profiles were obtained on the Greenland Ice Core Project (GRIP) ice core using two different electrical methods. After correction for temperature and density, the electrical conductivity method (ECM) technique responds only to acidity, while dielectric profiling (DEP) responds to acid, ammonium, and chloride. Detailed chemistry on a section of glacial-age ice allows us to confirm the calibration factor for chloride in DEP. Acidity dominates the DEP variability in the Holocene, Allerod/Bolling, and larger interstadials; ammonium dominates in the Younger Dry as, while chloride is the major contributor in cold periods including smaller interstadials. From the electrical signals plotted on a linear timescale we can deduce the background (nonvolcanic) acidity of the ice, varying from always acidic in the Holocene to always alkaline in the cold periods. In the interstadials, the ice is close to neutral, with most of it acidic in larger interstadials, most of it alkaline in smaller ones, and rapid alternations within interstadials. It is not clear whether neutralization of individual acidic particles occurred in the atmosphere or whether acid and alkaline particles coexisted until deposition in the snowpack. The changes in acidity observed at GRIP apply at least to all of Greenland and probably to much of North America. There would have been ecological effects and important changes in the uptake of some chemicals onto ice. If acidic sulfate particles were neutralized and removed from the atmosphere, which remains uncertain, then there are atmospheric chemistry and radiative effects that require further investigation.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1029/96JC02223
Programmes:	BAS Programmes > Pre 2000 programme
ISSN:	01480227
Date made live:	10 Oct 2016 13:59 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/514783

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1029/96JC02223

Programmes:

BAS Programmes > Pre 2000 programme

ISSN:

01480227

Date made live:

10 Oct 2016 13:59 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/514783