commit c78988bad9f22c2d6ea8a76eac920b6f8488e1b7
parent 414d1a4886ac2bbc93a0d5858a8aa096706f61bb
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date: Thu, 21 Nov 2019 13:54:04 +0100
Remove erroneous sentence
Diffstat:
1 file changed, 0 insertions(+), 2 deletions(-)
diff --git a/continuum-granular-manuscript1.tex b/continuum-granular-manuscript1.tex
@@ -290,8 +290,6 @@ In rate-\emph{limited} experiments, the iterative procedure is only performed fo
\subsection{Simulation setup}
Parameter values and their references are listed in Table~\ref{tab:params}.
For the first experiment with variable water pressure, we apply a water-pressure forcing amplitude of 50 kPa that modulates effective stress at the top around 100 kPa (Fig.~\ref{fig:stick_slip}).
-Deformation of subglacial beds is
-
Many simulations are performed under both stress- and rate-controlled shear, which both idealize the driving glacier physics.
Real glacier settings likely fall somewhere in between, depending on how important basal friction is to the overall stress balance.
Stress-controlled conditions approximate a setting where ice flow directly responds to changes in subglacial strain rates.
