Document Type
Conference Proceeding
Publication Title
Annals of Glaciology
Rights and Access Note
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Publication Date
2004
First Page
545
Last Page
556
Volume Number
39
Abstract/ Summary
Sixteen high-resolution ice-core records from West Antarctica and South Pole are used to examine the spatial and temporal distribution of sulfate for the last 200 years. The preservation of seasonal layers throughout the length of each record results in a dating accuracy of better than 1 year based on known global-scale volcanic events. A dual transport source for West Antarctic sea-salt (ss) SO42- and excess (xs) SO42- is observed: lower-tropospheric for areas below 1000m elevation and mid-/upper-tropospheric/stratospheric for areas located above 1000m. Our XsSO(4)(2-) records with volcanic peaks removed do not display any evidence of an anthropogenic impact on West Antarctic SO42- concentrations but do reveal that a major climate transition takes place over West Antarctica at similar to 1940. Global-scale volcanic eruptions appear as significant peaks in the robust-spline residual xsSO(4)(2-) records from sites located above 1000 m elevation but do not appear in the residual records from sites located below 1000 m.
Repository Citation
Dixon, D.; Mayewski, Paul Andrew; Kaspari, S.; Sneed, Sharon B.; and Handley, M., "A 200 Year Sub-Annual Record of Sulfate in West Antarctica, from Sixteen Ice Cores" (2004). Earth Science Faculty Scholarship. 120.
https://digitalcommons.library.umaine.edu/ers_facpub/120
Citation/Publisher Attribution
Dixon, D, Mayewski, PA, Kaspari, S, Sneed, S, and Handley, M, 2004, A 200 Year Sub-Annual Record of Sulfate in West Antarctica, from Sixteen Ice Cores: Annals of Glaciology, Vol 39, 2005, v. 39, p. 545-556. Available on publisher's site at: http://www.ingentaconnect.com/content/igsoc/agl/2004/00000039/00000001/art00083
Publisher Statement
© Copyright 2004 by the International Glaciological Society
DOI
10.3189/172756404781814113
Version
publisher's version of the published document