The role of double-diffusive convection in basal melting of Antarctic ice shelves
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Publication:5073265
DOI10.1073/pnas.2007541118zbMath1485.86015OpenAlexW3128315698WikidataQ128524643 ScholiaQ128524643MaRDI QIDQ5073265
Benjamin Keith Galton-Fenzi, Bishakhdatta Gayen, Madelaine Gamble Rosevear
Publication date: 5 May 2022
Published in: Proceedings of the National Academy of Sciences (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1073/pnas.2007541118
Diffusion (76R50) Direct numerical and large eddy simulation of turbulence (76F65) Glaciology (86A40) Mathematical modeling or simulation for problems pertaining to geophysics (86-10)
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Cites Work
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- Simulations of a double-diffusive interface in the diffusive convection regime
- Simulation of convection at a vertical ice face dissolving into saline water
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- Ablation of sloping ice faces into polar seawater
- Time-dependent fluxes across double-diffusive interfaces
- The role of double-diffusive convection in basal melting of Antarctic ice shelves
- Enhanced ablation of a vertical ice wall due to an external freshwater plume
- Double-Diffusive Convection
- Internal gravity waves generated by a turbulent bottom Ekman layer
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