Dried, closed-path eddy covariance method for measuring  carbon dioxide flux over sea ice

Butterworth, Brian J.; Else, Brent G. T.

doi:https://doi.org/10.5194/amt-11-6075-2018

Articles | Volume 11, issue 11

https://doi.org/10.5194/amt-11-6075-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/amt-11-6075-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 11, issue 11

Research article

|

09 Nov 2018

Research article |

| 09 Nov 2018

Dried, closed-path eddy covariance method for measuring carbon dioxide flux over sea ice

Brian J. Butterworth and Brent G. T. Else

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Final revised paper (published on 09 Nov 2018)
Supplement to the final revised paper
Preprint (discussion started on 31 Jul 2018)
Supplement to the preprint

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Reviewer 2', Anonymous Referee #2, 29 Sep 2018
- AC1: 'response to reviewer 2', Brian Butterworth, 17 Oct 2018
RC2: 'Review: Dried, closed-path eddy covariance method for measuring carbon dioxide flux over sea ice', John Prytherch, 03 Oct 2018
- AC2: 'response to reviewer 1', Brian Butterworth, 17 Oct 2018

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Brian Butterworth on behalf of the Authors (17 Oct 2018) Author's response Manuscript

ED: Publish as is (30 Oct 2018) by Christian Brümmer

Short summary

This study measured how quickly carbon dioxide was absorbed/released from sea ice to the air. We used a method that had never been tested over landlocked sea ice. To avoid water vapor ruining the carbon dioxide measurement, we dried the sample air before it went to the gas analyzer. This gave values that were more credible than those found by previous studies. We showed that this method will be useful for studying the processes which affect carbon dioxide exchange between sea ice and air.