예제 #1
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# += 0.05 #half block uplift

# pylab.figure(1)
# pylab.close()
#elev = mg['node']['topographic__elevation']
#elev_r = mg.node_vector_to_raster(elev)
# pylab.figure(1)
#im = pylab.imshow(elev_r, cmap=pylab.cm.RdBu)
# pylab.show()

# Display a message
print('Running ...')
start_time = time.time()

# instantiate the component:
diffusion_component = PerronNLDiffuse(mg, './drive_perron_params.txt')

# perform the loop:
elapsed_time = 0.  # total time in simulation
while elapsed_time < time_to_run:
    print(elapsed_time)
    if elapsed_time + dt < time_to_run:
        diffusion_component.input_timestep(dt)
    mg.at_node['topographic__elevation'][mg.core_nodes] += uplift * dt
    # mg.at_node['topographic__elevation'][mg.active_nodes[:(mg.active_nodes.shape[0]//2.)]] += uplift*dt #half block uplift
    # mg.at_node['topographic__elevation'][mg.active_nodes] += (numpy.arange(len(mg.active_nodes))) #nodes are tagged with their ID
    # pylab.figure(1)
    # pylab.close()
    #elev = mg['node']['topographic__elevation']
    #elev_r = mg.node_vector_to_raster(elev)
    # pylab.figure(1)
예제 #2
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mg.create_node_array_zeros('topographic_elevation')
z = mg.create_node_array_zeros() + leftmost_elev
z += initial_slope * np.amax(mg.node_y) - initial_slope * mg.node_y
#put these values plus roughness into that field
mg.at_node['topographic_elevation'] = z + np.random.rand(len(z)) / 100000.

#set up grid's boundary conditions (bottom, right, top, left is inactive)
mg.set_closed_boundaries_at_grid_edges(False, True, False, True)

# Display a message
print 'Running ...'

#instantiate the components:
fr = FlowRouter(mg)
sp = SPEroder(mg, input_file)
diffuse = PerronNLDiffuse(mg, input_file)
lin_diffuse = DiffusionComponent(grid=mg, input_stream=input_file)

#perform the loops:
for i in xrange(nt):
    #note the input arguments here are not totally standardized between modules
    #mg = diffuse.diffuse(mg, i*dt)
    mg = lin_diffuse.diffuse(mg, dt)
    mg = fr.route_flow(grid=mg)
    mg = sp.erode(mg)

    ##plot long profiles along channels
    pylab.figure(6)
    profile_IDs = prf.channel_nodes(mg, mg.at_node['steepest_slope'],
                                    mg.at_node['drainage_area'],
                                    mg.at_node['upstream_ID_order'],
예제 #3
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# create the field
mg.add_zeros('topographic__elevation', at='node')
# in our case, slope is zero, so the leftmost_elev is the mean elev
z = mg.zeros(at='node') + leftmost_elev
# put these values plus roughness into that field
mg['node']['topographic__elevation'] = z + np.random.rand(len(z)) / 100000.

# set up its boundary conditions (bottom, left, top, right)
# The mechanisms for this are all automated within the grid object
mg.set_fixed_value_boundaries_at_grid_edges(True, True, True, True)

# Display a message
print('Running ...')

# instantiate the components:
diffuse = PerronNLDiffuse(mg, input_file)
lin_diffuse = LinearDiffuser(grid=mg, input_stream=input_file)
# lin_diffuse.initialize(input_file)

# Perform the loops.
# First, we do the nonlinear diffusion:

# We're going to perform a block uplift of the interior of the grid, but
# leave the boundary nodes at their original elevations.
# access this function of the grid, and store the output with a local name
uplifted_nodes = mg.get_core_nodes()
#(Note: Node numbering runs across from the bottom left of the grid.)

# nt is the number of timesteps we calculated above, i.e., loop nt times.
# We never actually use i within the loop, but we could do.
for i in range(nt):
예제 #4
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mg = RasterModelGrid(nrows, ncols, dx)
# mg.set_looped_boundaries(True, True)
mg.set_closed_boundaries_at_grid_edges(True, True, True, True)

#create the fields in the grid
mg.create_node_array_zeros('topographic__elevation')
z = mg.create_node_array_zeros() + init_elev
mg.at_node['topographic__elevation'] = z + numpy.random.rand(len(z)) / 1000.

# Display a message
print('Running ...')
start_time = time.time()

#instantiate the component:
diffusion_component = PerronNLDiffuse(mg, './drive_perron_params.txt')

#perform the loop:
elapsed_time = 0.  #total time in simulation
while elapsed_time < time_to_run:
    print elapsed_time
    if elapsed_time + dt < time_to_run:
        diffusion_component.input_timestep(dt)
    mg.at_node['topographic__elevation'][mg.active_nodes[:(
        mg.active_nodes.shape[0] // 2.)]] += uplift * dt  #half block uplift

    mg = diffusion_component.diffuse(mg, elapsed_time)
    elapsed_time += dt

print('Total run time = ' + str(time.time() - start_time) + ' seconds.')
예제 #5
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##create the elevation field in the grid:
#create the field
mg.create_node_array_zeros('planet_surface__elevation')
z = mg.create_node_array_zeros() + leftmost_elev
z += initial_slope * np.amax(mg.node_y) - initial_slope * mg.node_y
#put these values plus roughness into that field
mg['node']['planet_surface__elevation'] = z + np.random.rand(len(z)) / 100000.

# Display a message
print 'Running ...'

#instantiate the components:
fr = FlowRouter(mg)
sp = SPEroder(mg, input_file)
diffuse = PerronNLDiffuse(mg, input_file)
lin_diffuse = DiffusionComponent(grid=mg)
lin_diffuse.initialize(input_file)

#perform the loops:
for i in xrange(nt):
    mg['node']['planet_surface__elevation'][
        mg.get_interior_nodes()] += uplift_per_step
    mg = fr.route_flow(grid=mg)
    mg = sp.erode(mg)
    mg = diffuse.diffuse(mg, i * dt)
    #mg = lin_diffuse.diffuse(mg, dt)

    ##plot long profiles along channels
    pylab.figure(6)
    profile_IDs = prf.channel_nodes(mg, mg.at_node['steepest_slope'],
예제 #6
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##create the elevation field in the grid:
#create the field
mg.create_node_array_zeros('planet_surface__elevation')
z = mg.create_node_array_zeros() + leftmost_elev
z += initial_slope*np.amax(mg.node_y) - initial_slope*mg.node_y
#put these values plus roughness into that field
mg['node'][ 'planet_surface__elevation'] = z + np.random.rand(len(z))/100000.

# Display a message
print 'Running ...' 

#instantiate the components:
fr = FlowRouter(mg)
sp = SPEroder(mg, input_file)
diffuse = PerronNLDiffuse(mg, input_file)
lin_diffuse = DiffusionComponent(grid=mg)
lin_diffuse.initialize(input_file)


#perform the loops:
for i in xrange(nt):
    mg['node']['planet_surface__elevation'][mg.get_interior_nodes()] += uplift_per_step
    mg = fr.route_flow(grid=mg)
    mg = sp.erode(mg)
    mg = diffuse.diffuse(mg, i*dt)
    #mg = lin_diffuse.diffuse(mg, dt)
    
    ##plot long profiles along channels
    pylab.figure(6)
    profile_IDs = prf.channel_nodes(mg, mg.at_node['steepest_slope'],
예제 #7
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#The mechanisms for this are all automated within the grid object
mg.set_inactive_boundaries(False, False, False, False)

##create the elevation field in the grid:
#create the field
mg.create_node_array_zeros('planet_surface__elevation')
z = mg.create_node_array_zeros(
) + leftmost_elev  #in our case, slope is zero, so the leftmost_elev is the mean elev
#put these values plus roughness into that field
mg['node']['planet_surface__elevation'] = z + np.random.rand(len(z)) / 100000.

# Display a message
print 'Running ...'

#instantiate the components:
diffuse = PerronNLDiffuse(mg, input_file)
lin_diffuse = DiffusionComponent(grid=mg, input_stream=input_file)
#lin_diffuse.initialize(input_file)

#Perform the loops.
#First, we do the nonlinear diffusion:

#We're going to perform a block uplift of the interior of the grid, but leave the boundary nodes at their original elevations.
uplifted_nodes = mg.get_core_nodes(
)  #access this function of the grid, and store the output with a local name
#(Note: Node numbering runs across from the bottom left of the grid.)

for i in xrange(
        nt
):  #nt is the number of timesteps we calculated above, i.e., loop nt times. We never actually use i within the loop, but we could do.
    #("xrange" is a clever memory-saving way of producing consecutive integers to govern a loop)