landlab.components.taylor_nonlinear_hillslope_flux.taylor_nonlinear_hillslope_flux¶
TaylorNonLinearDiffuser Component.
@author: R Glade @author: K Barnhart @author: G Tucker
- class TaylorNonLinearDiffuser[source]¶
Bases:
Component
Hillslope evolution using a Taylor Series expansion of the Andrews- Bucknam formulation of nonlinear hillslope flux derived following following Ganti et al., 2012. The flux is given as:
qs = KS * (1 + (S / Sc)**2 + (S / Sc)**4 + ... + (S / Sc)**2(n - 1))
where K is is the diffusivity, S is the slope, Sc is the critical slope, and n is the number of terms.
The default behavior uses two terms to produce a flux law as described by Equation 6 of Ganti et al., (2012).
Examples
>>> import numpy as np >>> import decimal >>> from landlab import RasterModelGrid >>> from landlab.plot.imshow import imshow_grid
>>> mg = RasterModelGrid((3, 3)) >>> z = mg.add_zeros("topographic__elevation", at="node") >>> initial_slope = 1.0 >>> leftmost_elev = 1000.0 >>> z[:] = leftmost_elev >>> z[:] += (initial_slope * np.amax(mg.x_of_node)) - (initial_slope * mg.x_of_node) >>> mg.set_closed_boundaries_at_grid_edges(False, True, False, True) >>> cubicflux = TaylorNonLinearDiffuser(mg, slope_crit=0.1) >>> cubicflux.run_one_step(1.0) >>> np.allclose( ... mg.at_node["topographic__elevation"], ... np.array( ... [1002.0, 1001.0, 1000.0, 1002.0, 1001.0, 1000.0, 1002.0, 1001.0, 1000.0] ... ), ... ) True
The
TaylorNonLinearDiffuser
makes and moves soil at a rate proportional to slope, this means that there is a characteristic time scale for soil transport and an associated stability criteria for the timestep. The maximum characteristic time scale, Demax, is given as a function of the hillslope diffustivity, D, the maximum slope, Smax, and the critical slope Sc:Demax = D * ( 1 + (Smax / Sc) ** 2 + (Smax / Sc) ** 4 + ... + (Smax / Sc) ** (2 * (n - 1)) )
The maximum stable time step is given by:
dtmax = courant_factor * dx * dx / Demax
Where the courant factor is a user defined scale (default is 0.2), and dx is the length of the shortest link in the grid.
The
TaylorNonLinearDiffuser
has a boolean flag that permits a user to be warned if timesteps are too large for the slopes in the model grid (if_unstable="warn"
) and a boolean flag that turns on dynamic timesteppping (dynamic_dt=False
).>>> cubicflux = TaylorNonLinearDiffuser(mg, slope_crit=0.1, if_unstable="warn") >>> cubicflux.run_one_step(2.0) Topographic slopes are high enough such that the Courant condition is exceeded AND you have not selected dynamic timestepping with dynamic_dt=True. This may lead to infinite and/or nan values for slope, elevation, and soil depth. Consider using a smaller time step or dynamic timestepping. The Courant condition recommends a timestep of 0.2 or smaller.
Alternatively you can specify
if_unstable="raise"
, and a RuntimeError will be raised if this condition is not met.Next, lets do an example with dynamic timestepping.
>>> mg = RasterModelGrid((5, 5)) >>> z = mg.add_zeros("topographic__elevation", at="node")
We’ll use a steep slope.
>>> z += mg.node_x.copy() ** 2 >>> cubicflux = TaylorNonLinearDiffuser(mg, if_unstable="warn", dynamic_dt=False)
Lets try to move the soil with a large timestep. Without dynamic time steps, this gives a warning that we’ve exceeded the dynamic timestep size and should use a smaller timestep. We could either use the smaller timestep, or specify that we want to use a dynamic timestep.
>>> cubicflux.run_one_step(10.0) Topographic slopes are high enough such that the Courant condition is exceeded AND you have not selected dynamic timestepping with dynamic_dt=True. This may lead to infinite and/or nan values for slope, elevation, and soil depth. Consider using a smaller time step or dynamic timestepping. The Courant condition recommends a timestep of 0.004 or smaller.
Now, we’ll re-build the grid and do the same example with dynamic timesteps.
>>> mg = RasterModelGrid((5, 5)) >>> z = mg.add_zeros("topographic__elevation", at="node") >>> z += mg.node_x.copy() ** 2 >>> cubicflux = TaylorNonLinearDiffuser(mg, if_unstable="warn", dynamic_dt=True) >>> cubicflux.run_one_step(10.0) >>> np.any(np.isnan(z)) False
References
Required Software Citation(s) Specific to this Component
Barnhart, K., Glade, R., Shobe, C., Tucker, G. (2019). Terrainbento 1.0: a Python package for multi-model analysis in long-term drainage basin evolution. Geoscientific Model Development 12(4), 1267–1297. https://dx.doi.org/10.5194/gmd-12-1267-2019
Additional References
Ganti, V., Passalacqua, P., Foufoula-Georgiou, E. (2012). A sub-grid scale closure for nonlinear hillslope sediment transport models Journal of Geophysical Research: Earth Surface 117(F2). https://dx.doi.org/10.1029/2011jf002181
Initialize the TaylorNonLinearDiffuser.
- Parameters:
grid (ModelGrid) – Landlab ModelGrid object
linear_diffusivity (float, optional) – Hillslope diffusivity (m**2 / yr).
slope_crit (float, optional) – Critical slope.
nterms (int, optional) – Number of terms in the Taylor expansion. Two terms (the default) gives the behavior described in Ganti et al. (2012).
dynamic_dt (bool, optional) – Turn dynamic time-stepping on or off.
if_unstable ({'pass', 'warn', 'raise'}, optional) – Specify how potential instability due to slopes that are too high is handled.
courant_factor (float, optional) – Factor to identify stable time-step duration when using dynamic timestepping.
- __init__(grid, linear_diffusivity=1.0, slope_crit=1.0, nterms=2, dynamic_dt=False, if_unstable='pass', courant_factor=0.2)[source]¶
Initialize the TaylorNonLinearDiffuser.
- Parameters:
grid (ModelGrid) – Landlab ModelGrid object
linear_diffusivity (float, optional) – Hillslope diffusivity (m**2 / yr).
slope_crit (float, optional) – Critical slope.
nterms (int, optional) – Number of terms in the Taylor expansion. Two terms (the default) gives the behavior described in Ganti et al. (2012).
dynamic_dt (bool, optional) – Turn dynamic time-stepping on or off.
if_unstable ({'pass', 'warn', 'raise'}, optional) – Specify how potential instability due to slopes that are too high is handled.
courant_factor (float, optional) – Factor to identify stable time-step duration when using dynamic timestepping.
- static __new__(cls, *args, **kwds)¶
- cite_as = '\n @article{barnhart2019terrain,\n author = {Barnhart, Katherine R and Glade, Rachel C and Shobe, Charles M\n and Tucker, Gregory E},\n title = {{Terrainbento 1.0: a Python package for multi-model analysis in\n long-term drainage basin evolution}},\n doi = {10.5194/gmd-12-1267-2019},\n pages = {1267---1297},\n number = {4},\n volume = {12},\n journal = {Geoscientific Model Development},\n year = {2019},\n }\n '¶
- property coords¶
Return the coordinates of nodes on grid attached to the component.
- property current_time¶
Current time.
Some components may keep track of the current time. In this case, the
current_time
attribute is incremented. Otherwise it is set to None.- Return type:
current_time
- definitions = (('soil__flux', 'flux of soil in direction of link'), ('topographic__elevation', 'Land surface topographic elevation'), ('topographic__slope', 'gradient of the ground surface'))¶
- classmethod from_path(grid, path)¶
Create a component from an input file.
- property grid¶
Return the grid attached to the component.
- initialize_optional_output_fields()¶
Create fields for a component based on its optional field outputs, if declared in _optional_var_names.
This method will create new fields (without overwrite) for any fields output by the component as optional. New fields are initialized to zero. New fields are created as arrays of floats, unless the component also contains the specifying property _var_type.
- initialize_output_fields(values_per_element=None)¶
Create fields for a component based on its input and output var names.
This method will create new fields (without overwrite) for any fields output by, but not supplied to, the component. New fields are initialized to zero. Ignores optional fields. New fields are created as arrays of floats, unless the component specifies the variable type.
- Parameters:
values_per_element (int (optional)) – On occasion, it is necessary to create a field that is of size (n_grid_elements, values_per_element) instead of the default size (n_grid_elements,). Use this keyword argument to acomplish this task.
- input_var_names = ('topographic__elevation',)¶
- name = 'TaylorNonLinearDiffuser'¶
- optional_var_names = ()¶
- output_var_names = ('soil__flux', 'topographic__elevation', 'topographic__slope')¶
- run_one_step(dt)[source]¶
Advance cubic soil flux component by one time step of size dt.
- Parameters:
dt (float) – The imposed timestep.
- property shape¶
Return the grid shape attached to the component, if defined.
- soilflux(dt)[source]¶
Calculate soil flux for a time period, dt.
- Parameters:
dt (float) – The imposed timestep.
- unit_agnostic = True¶
- units = (('soil__flux', 'm^2/yr'), ('topographic__elevation', 'm'), ('topographic__slope', 'm/m'))¶
- classmethod var_definition(name)¶
Get a description of a particular field.
- Parameters:
name (str) – A field name.
- Returns:
A description of each field.
- Return type:
tuple of (name, *description*)
- classmethod var_help(name)¶
Print a help message for a particular field.
- Parameters:
name (str) – A field name.
- classmethod var_loc(name)¶
Location where a particular variable is defined.
- var_mapping = (('soil__flux', 'link'), ('topographic__elevation', 'node'), ('topographic__slope', 'link'))¶