Nicholson Canyon Simulation

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</source> </source>
-=== Creating Probes ===+=== Numerical "wave gauge" ===
-The height of the water+The height of the water is measured using the same technique as the [[Liu_et_al_Benchmark]]. Probes are placed two and one kilometre before the edge of the canyon, at the edge of the canyon, halfway along the sliding block, at the original edge of the sliding block, above the deepest point the the canyon, at the far edge of the canyon and one and two kilometres beyond the far edge of the canyon.

Revision as of 04:55, 9 August 2011

Contents

Problem Definition

These simulations are loosely based on the geometry of the Nicholson Canyon in Cook Strait. It assumes a simple sliding block with a prescribed velocity. This work is similar to that of the benchmark cases of Enet et al. and Liu et al. with the difference being that while the two benchmark cases involved laboratory scales this simulation involves realistic geophysical scales.

Two-Dimensional Simulations

These simulations are run as a 2D vertical slice (i.e. assuming that the canyon and landslide are infinitely long and that there is no movement in the along-canyon direction

Generating the Landslide Body Geometry

First we need to create a .gts object that is the sliding block. One difficulty is that we have to ensure that the block is very close to the edges of the domain while still all lying inside the domain (otherwise those points lying outside the domain get 'left behind'). In the two dimensional simulation we still need a three dimensional block to ensure that it properly intersects the domain. This is made by first creating points on the surface of the block using an .awk file and then triangulating them using the gts delaunay triangulation

# Generating points using .awk file
awk -f nicholson.awk > points.tmp
# Delaunay triangulation and transformation using gts tools
( wc points.tmp | awk '{print $1" 0 0"}'; cat points.tmp ) | gtsdelaunay -d | gtstransform --rx=-90 > nichol_test.gts
# Shifting points to the domain boundary
sed -e "s/ -0.0168/0/g" < nichol_test.gts > nichol_testout.gts


The .awk file used to generate the points is

BEGIN {
a=0.272
b=1.7
alpha=atan2(a,b);
h=a*cos(alpha);
l1=b*cos(alpha);
l2=a*sin(alpha);
 
for (k=0; k <= 100; k++) {
for (i=-1; i <= 100; i++) { printf("%5.4f %5.4f %5.4f\n",l1*i/100, -
0.85+1.7*k/100 , h*i/100) }
for (i=1; i <= 101; i++) { printf("%5.4f %5.4f %5.4f\n",l1+l2*i/100,
-0.85+1.7*k/100, h*(1-i/100)) }
}
 
 
dx=1.0e-4
k=0.
j=-1.
for (i=-1; i <= 100; i++) { printf("%5.4f %5.4f %5.4f\n",l1*i/100, -0.
85+1.7*k/100-dx,h*j/100) }
for (i=1; i <= 101; i++) { printf("%5.4f %5.4f %5.4f\n",l1+l2*i/100, -
0.85+1.7*k/100-dx,h*j/100) }
 
k=100.
for (i=-1; i <= 100; i++) { printf("%5.4f %5.4f %5.4f\n",l1*i/100, -0.
85+1.7*k/100+dx,h*j/100) }
for (i=1; i <= 101; i++) { printf("%5.4f %5.4f %5.4f\n",l1+l2*i/100, -
0.85+1.7*k/100+dx,h*j/100) }
}

Numerical "wave gauge"

The height of the water is measured using the same technique as the Liu_et_al_Benchmark. Probes are placed two and one kilometre before the edge of the canyon, at the edge of the canyon, halfway along the sliding block, at the original edge of the sliding block, above the deepest point the the canyon, at the far edge of the canyon and one and two kilometres beyond the far edge of the canyon.

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