commit a9f79ec4da5140331d52ada83cfa3ee030e1571c
parent edf97b34d7ba2dcd925192cd64479d16c4767b2a
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date:   Fri, 28 Jun 2019 17:00:43 +0200
Update figure paths, remove --time-step from README
Diffstat:
1 file changed, 5 insertions(+), 6 deletions(-)
diff --git a/README.md b/README.md
@@ -42,7 +42,6 @@ optional arguments:
  -H, --fluid-pressure-phase VAL  fluid pressure at +z edge [Pa] (default 0)
  -t, --time VAL                  simulation start time [s] (default 0)
  -T, --time-end VAL              simulation end time [s] (default 1)
- -D, --time-step VAL             computational time step length [s] (default 2)
  -I, --file-interval VAL         interval between output files [s] (default 0.1)
  -v, --version                   show version information
  -h, --help                      show this message
@@ -59,7 +58,7 @@ probably be improved further.
 | Discrete-element model  | Continuum Model |
 | ----------------------- | --------------- |
 | Damsgaard et al. 2013   |                 |
-|  |  |
+|  |  |
 
 ### Stress and strain rate
 The rheology is of Bingham type, where no deformation occurs beneath the 
@@ -71,15 +70,15 @@ have *b* = 0.94 ([Forterre and Pouliquen
 | Real material (laboratory or field study)    | Continuum Model |
 | -------------------------------------------- | --------------- |
 | Upstream-B ([Kamb 1991](https://doi.org/10.1029/91jb00946)): |                 |
-|  |  |
+|  |  |
 | Various subglacial tills ([Iverson 2010](https://doi.org/10.3189/002214311796406220)): |                 |
-|  |  |
+|  |  |
 | Whillans Ice Plain ([Tulaczyk 2006](https://doi.org/10.3189/172756506781828601)): |                 |
-|  |  |
+|  |  |
 
 ### Variable water pressure
 The model is expanded from the Henann and Kamrin 2013 model by including a 
 diffusive porewater pressure parameterization. Below is an example of diurnal 
 water-pressure variations that gradually propagate into the bed.
 
-
+