Carbonyl sulfide hydrolysis in antarctic ice cores and an atmospheric history for the last 8000 years

Carbonyl sulfide (COS) was measured in Antarctic ice core samples from the Byrd, Siple Dome, Taylor Dome, and West Antarctic Ice Sheet Divide sites covering the last 8000 years of the Holocene. COS levels decrease downcore in most of these ice cores. The magnitude of the downcore trends varies among...

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Bibliographic Details
Main Authors: Aydin, M, Fudge, TJ, Verhulst, KR, Nicewonger, MR, Waddington, ED, Saltzman, ES
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 2014
Subjects:
Online Access:https://escholarship.org/uc/item/6kn3w9qr