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...

Full description

Bibliographic Details
Published in:The Cryosphere
Main Authors: C. Buizert, J. P. Severinghaus
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2016
Subjects:
Online Access:https://doi.org/10.5194/tc-10-2099-2016
https://doaj.org/article/3bdf094c4fae4b8bac3896c1fd0b7d51