The effect of meltwater plumes on the melting of a vertical glacier face

Kimura, Satoshi ORCID: https://orcid.org/0000-0003-1689-1605; Holland, Paul R. ORCID: https://orcid.org/0000-0001-8370-289X; Jenkins, Adrian ORCID: https://orcid.org/0000-0002-9117-0616; Piggott, Matthew. 2014 The effect of meltwater plumes on the melting of a vertical glacier face. Journal of Physical Oceanography, 44 (12). 3099-3117. https://doi.org/10.1175/JPO-D-13-0219.1

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Abstract/Summary

Freshwater produced by the surface melting of ice sheets is commonly discharged into ocean fjords from the bottom of deep fjord-terminating glaciers. The discharge of the freshwater forms upwelling plumes in front of the glacier calving face. We simulate the meltwater plumes emanated into an unstratified environment using a non-hydrostatic ocean model with an unstructured mesh and subgrid-scale mixing calibrated by comparison to established plume theory. The presence of an ice face reduces the entrainment of seawater into the meltwater plumes, so the plumes remain attached to the ice front, in contrast to previous simple models. Ice melting increases with height above the discharge, also in contrast to some simple models, and we speculate that this ‘overcutting’ may contribute to a tendency of icebergs to topple inwards toward the ice face upon calving. The overall melt rate is found to increase with discharge flux only up to a critical value, which depends on the channel size. The melt rate is not a simple function of the subglacial discharge flux, as assumed by many previous studies. For a given discharge flux, the geometry of the plume source also significantly affects the melting, with higher melt rates obtained for a thinner, wider source. In a wider channel, two plumes are emanated near the source and these plumes eventually coalesce. Such merged meltwater plumes ascend faster and increase the maximum melt rate near the center of the channel. The melt rate per unit discharge decreases as the subglacial system becomes more channelised.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1175/JPO-D-13-0219.1
Programmes:	BAS Programmes > Polar Science for Planet Earth (2009 - ) > Polar Oceans
ISSN:	0022-3670
Additional Keywords:	geographic location, ice sheets, circulation/dynamics, buoyancy, ocean dynamics, vertical motion, models and modeling, ocean models
Date made live:	24 Sep 2014 10:08 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/508481

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