commit 8c17a90f2fa706c8b0294282628df489238ddec5
parent 2faacb3f20d411154809cdbe5fa201c569e1155c
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date: Thu, 17 Dec 2020 16:46:00 +0100
commsenv: small tweaks before publication
Diffstat:
2 files changed, 32 insertions(+), 29 deletions(-)
diff --git a/pages/008-commsenv.html b/pages/008-commsenv.html
@@ -3,28 +3,30 @@ 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
+was 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>
+Antarctic ice sheets, but also smaller glaciers in the mountainous
+areas of Alaska, northern Scandinavia, and elsewhere. The movement
+of sediment could be important for the progression of glaciations,
+and influence 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 &
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
+with co-authors <a
+href="https://sites.google.com/site/gorenliran/home">Liran Goren</a>,
+University of the Negev (Israel), and <a
+href="https://profiles.stanford.edu/jenny-suckale">Jenny Suckale</a>,
+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 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>
@@ -64,7 +66,7 @@ preparation of this paper:</p>
<h2>Links and references:</h2>
<ul>
- <li><a href="">Publication on journal webpage</a></li>
+ <li><a href="https://doi.org/10.1038/s43247-020-00074-7">Publication on journal webpage</a> (open access)</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>
diff --git a/pages/008-commsenv.txt b/pages/008-commsenv.txt
@@ -2,15 +2,15 @@ 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
+North America, and in the forelands of the Alps, the landscape was
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.
+Antarctic ice sheets, but also smaller glaciers in the mountainous
+areas of Alaska, northern Scandinavia, and elsewhere. The movement
+of sediment could be important for the progression of glaciations,
+and influence how resilient marine-terminating ice streams are
+against sea-level rise.
Today, the Nature-group journal Communications Earth & Environment
published my paper on sediment beneath ice. Together with co-authors
@@ -18,11 +18,11 @@ 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 cngf-pf for the simulations.
+provide a way 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
+cngf-pf for the simulations.
## Abstract
@@ -63,7 +63,8 @@ preparation of this paper:
## Links and references:
- - Publication on journal webpage:
+ - Publication on journal webpage (open access):
+ https://doi.org/10.1038/s43247-020-00074-7
- Article PDF (?? MB):
- Supplementary information PDF (?? MB):
- Source code for producing figures: git://src.adamsgaard.dk/cngf-pf-exp1
