The role of regional feedbacks in glacial inception on Baffin Island: the interaction of ice flow and meteorology

Birch, Leah; Cronin, Timothy; Tziperman, Eli

doi:https://doi.org/10.5194/cp-14-1441-2018

Articles | Volume 14, issue 10

https://doi.org/10.5194/cp-14-1441-2018

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

https://doi.org/10.5194/cp-14-1441-2018

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

Articles | Volume 14, issue 10

Research article

|

18 Oct 2018

Research article |

| 18 Oct 2018

The role of regional feedbacks in glacial inception on Baffin Island: the interaction of ice flow and meteorology

Leah Birch, Timothy Cronin, and Eli Tziperman

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Final revised paper (published on 18 Oct 2018)
Supplement to the final revised paper
Preprint (discussion started on 07 Feb 2018)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Review of "Glacial inception on Baffin Island: the interaction of ice flow and meteorology"', Anonymous Referee #1, 05 Mar 2018
- AC1: 'Response to Reviewers', Leah Birch, 15 May 2018
RC2: 'More analysis needed', Anonymous Referee #2, 17 Apr 2018
- AC1: 'Response to Reviewers', Leah Birch, 15 May 2018

Peer-review completion

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

ED: Reconsider after major revisions (16 May 2018) by Marit-Solveig Seidenkrantz

AR by Leah Birch on behalf of the Authors (27 Jun 2018) Author's response Manuscript

ED: Referee Nomination & Report Request started (28 Jun 2018) by Marit-Solveig Seidenkrantz

RR by Anonymous Referee #1 (16 Jul 2018)

ED: Publish subject to technical corrections (17 Sep 2018) by Marit-Solveig Seidenkrantz

Short summary

We investigate the regional dynamics at the beginning of the last ice age, using a nested configuration of the Weather Research and Forecasting (WRF) model with a simple ice flow model. We find that ice sheet height causes a negative feedback on continued ice growth by interacting with the atmospheric circulation, causing warming on Baffin Island, and inhibiting the initiation of the last ice age. We conclude that processes at larger scales are needed to overcome the regional warming effect.