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<!DOCTYPE HTML>
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<title>Just Swimmingly - Research</title>
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<h1><strong>Stefanie Mack, PhD</strong><br />
Scientist, Oceanographer<br />
Currently at the British Antarctic Survey</h1>
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<h2>Research</h2>
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<a href="Media/CoupledModels.png" class="image fit thumb"><img src="Media/CoupledModels.png" alt="" /></a>
<h3>Modeling ocean-ice shelf interactions</h3>
<p>One of the largest uncertainties in future sea level rise projections is how much the Antarctic Ice Sheet will contribute. The mass of the Antarctic Ice Sheet is held in place through the "buttressing" effect of floating ice shelves. Acting as a cork, these ice shelves help control the flow of ice from the continent. A collapse of one, or several, ice shelves could potentially trigger a large amount of ice lost from the Antarctic Ice Sheet and a subsequent rise in sea level. The stability of ice shelves depends on their geometry, including their thickness and shape, as well as the geometry of the bedrock below the ice and the position of the grounding line - where the ice begins to float. Changes to the basal melt rates of these ice shelves, driven by the ocean, can affect their stability. I am building an ocean model domain of an ice shelf cavity and working with ice shelf modelers to couple the ocean and ice models. Our objectives are to answer technical questions about the model coupling process, and to answer scientific questions about how ocean-ice interactions affect ice shelf stability.</p>
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<h3>Antarctic Cyclones: Expression in Sea-ice (ACES)</h3>
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<li><a href="https://www.bas.ac.uk/profile/steck" class="button">BAS Research Profile</a></li>
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