tcommsenv: minor grammar changes - adamsgaard.dk - my academic webpage | |
git clone git://src.adamsgaard.dk/adamsgaard.dk | |
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--- | |
commit dd31eae4794c13f020bf9e41616e4594f8fd7014 | |
parent 71e975f0e66fccea5b8de7db332845b8126b9c3c | |
Author: Anders Damsgaard <[email protected]> | |
Date: Fri, 18 Dec 2020 12:43:34 +0100 | |
commsenv: minor grammar changes | |
Diffstat: | |
M pages/008-commsenv.html | 2 +- | |
M pages/008-commsenv.txt | 15 +++++++-------- | |
2 files changed, 8 insertions(+), 9 deletions(-) | |
--- | |
diff --git a/pages/008-commsenv.html b/pages/008-commsenv.html | |
t@@ -4,7 +4,7 @@ glacial meltwater, and their lubrication accelerates the ice m… | |
In formerly-glaciated areas of the world, for example Northern | |
Europe, 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 | |
+with its flow. Sediment movement is also observed under current | |
glaciers, both the fast-moving ice streams of the Greenland and | |
Antarctic ice sheets, but also smaller glaciers in the mountainous | |
areas of Alaska, northern Scandinavia, and elsewhere. The movement | |
diff --git a/pages/008-commsenv.txt b/pages/008-commsenv.txt | |
t@@ -4,20 +4,19 @@ meltwater, and their lubrication accelerates the ice movemen… | |
formerly-glaciated areas of the world, for example Northern Europe, | |
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, 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. | |
+its flow. Sediment movement is also observed under current glaciers, | |
+both the fast-moving ice streams of the Greenland and 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 | |
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 | |
+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 |