Articles | Volume 14, issue 7
https://doi.org/10.5194/tc-14-2515-2020
https://doi.org/10.5194/tc-14-2515-2020
Research article
 | 
31 Jul 2020
Research article |  | 31 Jul 2020

The contrasting response of outlet glaciers to interior and ocean forcing

John Erich Christian, Alexander A. Robel, Cristian Proistosescu, Gerard Roe, Michelle Koutnik, and Knut Christianson

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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (22 May 2020) by Olivier Gagliardini
AR by John Erich Christian on behalf of the Authors (28 May 2020)  Author's response   Manuscript 
ED: Publish as is (19 Jun 2020) by Olivier Gagliardini
AR by John Erich Christian on behalf of the Authors (23 Jun 2020)
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Short summary
We use simple, physics-based models to compare how marine-terminating glaciers respond to changes at their marine margin vs. inland surface melt. Initial glacier retreat is more rapid for ocean changes than for inland changes, but in both cases, glaciers will continue responding for millennia. We analyze several implications of these differing pathways of change. In particular, natural ocean variability must be better understood to correctly identify the anthropogenic role in glacier retreat.