manus_continuum_granular1

commit 5bcef91fe3263298875ead8ddcfff9a26490b882
parent 42bf9843466496adbefb06de4726d4138671d3eb
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date:   Thu, 10 Oct 2019 19:08:43 +0200

Fix references and update repo link in appendix

Diffstat:
M
BIBnew.bib
 | 
13
+------------
M
continuum-granular-manuscript1.tex
 | 
4
++--

2 files changed, 3 insertions(+), 14 deletions(-)
diff --git a/BIBnew.bib b/BIBnew.bib
@@ -148,17 +148,6 @@
 	Publisher                = {Elsevier}
 }
 
-@Article{Bagnold1954,
-	Title                    = {Experiments on a gravity-free dispersion of large solid spheres in a {N}ewtonian fluid under shear},
-	Author                   = {Bagnold, R. A.},
-	Journal                  = {Proceedings of the Royal society of London. Series A, Mathematical and Physical Sciences},
-	Year                     = {1954},
-	Number                   = {1160},
-	Pages                    = {49--63},
-	Volume                   = {225},
-	Publisher                = {JSTOR}
-}
-
 @Article{Bailey1989,
 	Title                    = {A soil compaction model for cylindrical stress states},
 	Author                   = {Bailey, A. C. and Johnson, C. E.},
@@ -9173,7 +9162,7 @@ Winton and A. T. Wittenberg and F. Zeng and R. Zhang and J. P. Dunne},
 	journal = {{GFF}}
 }
 
-@article{Hermanowski2019,
+@article{Hermanowski2019b,
 	doi = {10.1029/2018jf004939},
 	year = 2019,
 	month = {jul},
diff --git a/continuum-granular-manuscript1.tex b/continuum-granular-manuscript1.tex
@@ -515,7 +515,7 @@ The response in maximum deformation depth is non-linear for triangular perturbat
 The stress-dependt sediment advection observed in Fig.~\ref{fig:strain_distribution} is relevant for instability theories of subglacial landform development \citep{Hindmarsh1999, Fowler2000, Schoof2007, Fowler2018}.
 From geometrical considerations, it is likely that bed-normal stresses on the stoss side of subglacial topography are higher than on the lee side.
 With all other physical conditions being equal, our results indicate that shear-driven sediment advection would be larger on the stoss side of bed perturbations than behind them.
-Topography of non-planar ice-bed interfaces (proto-drumlins, ribbed moraines, etc.) may be transported and modulated through the variable transport capacity, unless stress differences are overprinted by spatial variations in water pressure \citep[e.g.][]{Sergienko2013, McCracken2016, Iverson2017b, Hermanowski2019}.
+Topography of non-planar ice-bed interfaces (proto-drumlins, ribbed moraines, etc.) may be transported and modulated through the variable transport capacity, unless stress differences are overprinted by spatial variations in water pressure \citep[e.g.][]{Sergienko2013, McCracken2016, Iverson2017b, Hermanowski2019b}.
 
 Previously, \citet{Iverson2001} modeled the subglacial bed as a series of parallel Coulomb-frictional slabs.
 They demonstrated that random perturbations in effective stress at depth can distribute deformation away from the ice-bed interface.
@@ -577,7 +577,7 @@ Similarly, sudden water-pressure pulses are powerful drivers for single events o
 \label{sec:appendix}
 The grain-water model is written in C and is available under free-software licensing at \url{https://src.adamsgaard.dk/1d_fd_simple_shear}.
 All simulation parameters can be specified as command-line arguments.
-The results and figures in this paper can be reproduced by following the instructions in the experiment repository for this publication, available at \url{https://src.adamsgaard.dk/.manus_continuum_granular1_exp}.
+The results and figures in this paper can be reproduced by following the instructions in the experiment repository for this publication, available at \url{https://src.adamsgaard.dk/manus_continuum_granular1_exp}.
 
 %% Bibliography
 \printbibliography{}