Dispersion in deep polar firn driven by synoptic-scale surface pressure variability

Commonly, three mechanisms of firn air transport are distinguished: molecular diffusion, advection, and near-surface convective mixing. Here we identify and describe a fourth mechanism, namely dispersion driven by synoptic-scale surface pressure variability (or barometric pumping). We use published...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Buizert, Christo, Severinghaus, Jeffrey P.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2016
Subjects:
Online Access:https://doi.org/10.5194/tc-10-2099-2016
https://noa.gwlb.de/receive/cop_mods_00043314
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00042934/tc-10-2099-2016.pdf
https://tc.copernicus.org/articles/10/2099/2016/tc-10-2099-2016.pdf