tadd post on commsenv paper, wait for publication - adamsgaard.dk - my academic webpage
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 (HTM) Author: Anders Damsgaard <anders@adamsgaard.dk>
       Date:   Wed,  9 Dec 2020 11:04:28 +0100
       
       add post on commsenv paper, wait for publication
       
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       +filename=commsenv.html
       +title=New paper out on the coupled dynamics of ice, meltwater, and till
       +description=A brief summary of my new paper published in Communications Earth & Environment
       +id=commsenv
       +tags=science, glaciology, ice sheet
       +created=2020-12-09
       +updated=2020-12-09
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       +<p>The majority of glaciers and ice sheets flow on a bed of loose
       +and thawed sediments.  These sediments are weakened by pressurized
       +glacial meltwater, and their lubrication accelerates the ice movement.
       +In formerly-glaciated areas of the world, for example Northern
       +Europe, North America, and in the forelands of the Alps, the landscape
       +is reshaped and remolded by past ice moving the sediments along
       +with its flow.  The sediment movement is also observed under current
       +glaciers, both the fast-moving ice streams of the Greenland and
       +Antarctic ice sheets, as well as smaller glaciers in the mountainous
       +areas of Alaska, northern Sweden, and elsewhere.  The movement of
       +sediment could be important for the past progression of glaciations,
       +and how resilient marine-terminating ice streams are against sea-level
       +rise.</p>
       +
       +<p>Today, the Nature-group journal <a
       +href="https://www.nature.com/commsenv/">Communications Earth &amp;
       +Environment</a> published my paper on sediment beneath ice.  Together
       +with co-authors Liran Goren, University of the Negev (Israel), and
       +Jenny Suckale, Stanford University (California, USA), we present a
       +new computer model that simulates the coupled mechanical behavior
       +of ice, sediment, and meltwater.  We calibrate the model against
       +real materials, and provide a way forward for including sediment
       +transport in ice-flow models.  We also show that water-pressure
       +variations with the right frequency can create create very weak
       +sections inside the bed, and this greatly enhances sediment transport.
       +I designed the freely-available program <a
       +href="https://src.adamsgaard.dk/cngf-pf">cngf-pf</a> for the
       +simulations.</p>
       +
       +<h2>Abstract</h2>
       +<blockquote>
       +<b>Water pressure fluctuations control variability in sediment flux
       +and slip dynamics beneath glaciers and ice streams</b>
       +<br><br>
       +Rapid ice loss is facilitated by sliding over beds consisting of
       +reworked sediments and erosional products, commonly referred to as
       +till. The dynamic interplay between ice and till reshapes the bed,
       +creating landforms preserved from past glaciations. Leveraging the
       +imprint left by past glaciations as constraints for projecting
       +future deglaciation is hindered by our incomplete understanding of
       +evolving basal slip. Here, we develop a continuum model of
       +water-saturated, cohesive till to quantify the interplay between
       +meltwater percolation and till mobilization that governs changes
       +in the depth of basal slip under fast-moving ice. Our model explains
       +the puzzling variability of observed slip depths by relating localized
       +till deformation to perturbations in pore-water pressure. It
       +demonstrates that variable slip depth is an inherent property of
       +the ice-meltwater-till system, which could help understand why some
       +paleo-landforms like grounding-zone wedges appear to have formed
       +quickly relative to current till-transport rates.
       +</blockquote>
       +
       +<h2>Metrics</h2>
       +<p>It is a substantial task to prepare a scientific publication.  The
       +commit counts below mark the number of revisions done during
       +preparation of this paper:</p>
       +
       +<ul>
       +        <li>Main article text: 239 commits</li>
       +        <li>Supplementary information text: 35 commits</li>
       +        <li>Experiments and figures: 282 commits</li>
       +        <li>Simulation software: 354 commits</li>
       +</ul>
       +
       +<h2>Links and references:</h2>
       +<ul>
       +        <li><a href="">Publication on journal webpage</a></li>
       +        <li><a href="">Article PDF</a> (?? MB)</li>
       +        <li><a href="">Supplementary information PDF</a> (?? MB)</li>
       +        <li><a href="https://src.adamsgaard.dk/cngf-pf-exp1">Source code for producing figures</a></li>
       +        <li><a href="https://src.adamsgaard.dk/cngf-pf">Simulation software</a></li>
       +</ul>