Articles | Volume 18, issue 1
https://doi.org/10.5194/tc-18-265-2024
https://doi.org/10.5194/tc-18-265-2024
Brief communication
 | 
12 Jan 2024
Brief communication |  | 12 Jan 2024

Brief communication: A technique for making in situ measurements at the ice–water boundary of small pieces of floating glacier ice

Hayden A. Johnson, Oskar Glowacki, Grant B. Deane, and M. Dale Stokes

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Cited articles

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Cowton, T., Slater, D., Sole, A., Goldberg, D., and Nienow, P.: Modeling the impact of glacial runoff on fjord circulation and submarine melt rate using a new subgrid-scale parameterization for glacial plumes, J. Geophys. Res.-Oceans, 120, 796–812, 2015. a
Davison, B., Cowton, T., Cottier, F. R., and Sole, A.: Iceberg melting substantially modifies oceanic heat flux towards a major Greenlandic tidewater glacier, Nat. Commun., 11, 5983, https://doi.org/10.1038/s41467-020-19805-7, 2020. a
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Hellmer, H. H. and Olbers, D. J.: A two-dimensional model for the thermohaline circulation under an ice shelf, Antarct. Sci., 1, 325–336, 1989. a
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Short summary
This paper is about a way to make measurements close to small pieces of floating glacier ice. This is done by attaching instruments to the ice from a small boat. Making these measurements will be helpful for the study of the physics that goes on at small scales when glacier ice is in contact with ocean water. Understanding these small-scale physics may ultimately help improve our understanding of how much ice in Greenland and Antarctica will melt as a result of warming oceans.
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