1. Double‐Diffusive Layer and Meltwater Plume Effects on Ice Face Scalloping in Phase‐Change Simulations.
- Author
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Wilson, Nicholas J., Vreugdenhil, Catherine A., Gayen, Bishakhdatta, and Hester, Eric W.
- Subjects
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ICE shelves , *MELTWATER , *ICE , *ANTARCTIC ice , *OCEAN dynamics , *OCEAN temperature , *SCALLOPS - Abstract
Antarctic ice shelves are losing mass at increasing rates, yet the ice‐ocean interactions that cause significant ice loss are not well understood. A new approach of high‐resolution phase‐change simulations is used to model vertical ice melting into a stratified ocean. The ocean dynamics show complicated interplay between a turbulent buoyant meltwater plume and double‐diffusive layers, while the ice actively melts and changes topography. At room temperatures, the double‐diffusive layer thickness is closely linked to ice scalloping. At lower, more realistic ocean temperatures, the meltwater plume becomes prominent with a laminar‐to‐turbulent transition imprinting an indent on the melting ice. The double‐diffusive layer thickness is consistent with scaling prediction, while the real‐world application demonstrates reasonably good matching of the scaling prediction for some Antarctic regions. Our study is a key first step toward the future use of high‐resolution phase‐change fluid dynamics simulations to better understand Antarctic ice shelves in a changing climate. Plain Language Summary: Future climate scenarios and sea level rise are closely tied to the accelerating loss of Antarctic ice shelves, which lose significant mass by melting into the surrounding ocean. However, the extent of ice shelf mass loss in a changing climate is currently not well understood, with lack of knowledge on the fine‐scale ice‐ocean interactions presenting a key restriction on the accuracy of climate predictions. Here, we use a new suite of numerical computer simulations to model an ice face melting into the ocean. In particular, our simulations allow the ice face to melt back and change shape, which previous numerical simulations could not attempt. We see interesting ocean dynamics known as "double‐diffusive layers" that occur because temperature and salinity both affect the water density. In addition, we also see a buoyant meltwater plume evolve next to the ice face. Both the double‐diffusive layers and meltwater plume can influence the ice melting and shape. Our results are a first step in using these new phase‐change simulations to model ice‐ocean interactions, and will help to better understand the Antarctic response to a changing climate. Key Points: High‐resolution phase‐change simulations are used to examine a vertical ice face melting into a stratified ocean at low temperaturesA distinct laminar‐to‐turbulent transition occurs in the meltwater plume as it rises, accompanied by an indent in the ice at the transitionDouble‐diffusive layers adjacent to the turbulent plume are consistent with scaling predictions and are relevant to the ocean application [ABSTRACT FROM AUTHOR]
- Published
- 2023
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