tcommsenv: minor grammar changes - adamsgaard.dk - my academic webpage
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 (DIR) commit dd31eae4794c13f020bf9e41616e4594f8fd7014
 (DIR) parent 71e975f0e66fccea5b8de7db332845b8126b9c3c
 (HTM) Author: Anders Damsgaard <anders@adamsgaard.dk>
       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(-)
       ---
 (DIR) 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 movement.
        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
 (DIR) diff --git a/pages/008-commsenv.txt b/pages/008-commsenv.txt
       t@@ -4,20 +4,19 @@ 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 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