tcommsenv: small tweaks before publication - adamsgaard.dk - my academic webpage | |
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commit 8c17a90f2fa706c8b0294282628df489238ddec5 | |
parent 2faacb3f20d411154809cdbe5fa201c569e1155c | |
Author: Anders Damsgaard <[email protected]> | |
Date: Thu, 17 Dec 2020 16:46:00 +0100 | |
commsenv: small tweaks before publication | |
Diffstat: | |
M pages/008-commsenv.html | 36 ++++++++++++++++-------------… | |
M pages/008-commsenv.txt | 25 +++++++++++++------------ | |
2 files changed, 32 insertions(+), 29 deletions(-) | |
--- | |
diff --git a/pages/008-commsenv.html b/pages/008-commsenv.html | |
t@@ -3,28 +3,30 @@ and thawed sediments. These sediments are weakened by press… | |
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> | |
t@@ -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 o… | |
<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 p… | |
diff --git a/pages/008-commsenv.txt b/pages/008-commsenv.txt | |
t@@ -2,15 +2,15 @@ The majority of glaciers and ice sheets flow on a bed of loo… | |
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 | |
t@@ -18,11 +18,11 @@ Liran Goren, University of the Negev (Israel), and Jenny S… | |
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 | |
t@@ -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 |