Articles | Volume 14, issue 6
The Cryosphere, 14, 1951–1969, 2020
https://doi.org/10.5194/tc-14-1951-2020
The Cryosphere, 14, 1951–1969, 2020
https://doi.org/10.5194/tc-14-1951-2020

Research article 18 Jun 2020

Research article | 18 Jun 2020

Surface emergence of glacial plumes determined by fjord stratification

Eva De Andrés et al.

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (23 Apr 2020) by Jan De Rydt
AR by Eva De Andrés on behalf of the Authors (24 Apr 2020)  Author's response    Manuscript
ED: Publish subject to technical corrections (11 May 2020) by Jan De Rydt

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Eva De Andrés on behalf of the Authors (16 Jun 2020)   Author's adjustment   Manuscript
EA: Adjustments approved (16 Jun 2020) by Jan De Rydt
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Short summary
Buoyant plumes at tidewater glaciers result from localized subglacial discharges of surface melt. They promote glacier submarine melting and influence the delivery of nutrients to the fjord's surface waters. Combining plume theory with observations, we have found that increased fjord stratification, which is due to larger meltwater content, prevents the vertical growth of the plume and buffers submarine melting. We discuss the implications for nutrient fluxes, CO2 trapping and water export.