manus_continuum_granular1

commit 3e44a5a2cfb1e6e5a16c33ceb00d1a75eb626f4b
parent a7f0be01be04a19c219c757e98ea06eb7adb9809
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date:   Tue,  3 Dec 2019 16:15:53 +0100

Update keypoints

Diffstat:
M
continuum-granular-manuscript1.tex
 | 
2
+-

1 file changed, 1 insertion(+), 1 deletion(-)
diff --git a/continuum-granular-manuscript1.tex b/continuum-granular-manuscript1.tex
@@ -38,7 +38,7 @@
 
 \begin{keypoints}  % each keypoint max 140 chars
 \item Non-local continuum model is consistent with subglacial till rheology
-\item Sediment advection depends on the current stress and the history of water-pressure forcings
+\item Sediment advection depends on the subglacial stress and sediment properties
 \item Water-pressure perturbations can cause deep shear mobilization of till beneath the ice-bed interface
 \end{keypoints}