Articles | Volume 13, issue 11
Clim. Past, 13, 1685–1693, 2017
https://doi.org/10.5194/cp-13-1685-2017
Clim. Past, 13, 1685–1693, 2017
https://doi.org/10.5194/cp-13-1685-2017

Research article 24 Nov 2017

Research article | 24 Nov 2017

Critical porosity of gas enclosure in polar firn independent of climate

Christoph Florian Schaller et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by Editor) (16 Oct 2017) by Eric Wolff
AR by Christoph Florian Schaller on behalf of the Authors (17 Oct 2017)  Author's response    Manuscript
ED: Publish as is (20 Oct 2017) by Eric Wolff
Download
Short summary
In order to interpret the paleoclimatic record stored in the air enclosed in polar ice cores, it is crucial to understand the fundamental lock-in process. In our study, we present the first extensive data set of direct firn microstructure measurements and use it to show that the critical porosity of gas enclosure is independent of the climatic site conditions (such as temperature and accumulation rate). This leads to significant changes in dating and interpretation of ice-core gas records.