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.
-
+