landlab
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Landscape evolution and surface process modelling in Python. Build 2D numerical models for erosion, hydrology, soil transport, and geomorphology. Use when Claude needs to: (1) Model landscape evolution over time, (2) Simulate river/stream erosion, (3) Route water flow across terrain, (4) Model hillslope diffusion processes, (5) Simulate weathering and soil production, (6) Analyze drainage networks, (7) Combine multiple geomorphic processes, (8) Load/save DEM data for modeling.
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Quick Reference
python
from landlab import RasterModelGrid
from landlab.components import FlowAccumulator, StreamPowerEroder
import numpy as np
# Create grid
grid = RasterModelGrid((100, 100), xy_spacing=10.0)
z = grid.add_zeros('topographic__elevation', at='node')
z += np.random.rand(grid.number_of_nodes) * 0.1
# Set boundaries (open bottom edge)
grid.set_closed_boundaries_at_grid_edges(True, True, True, False)
# Create and run components
fa = FlowAccumulator(grid, flow_director='D8')
sp = StreamPowerEroder(grid, K_sp=1e-5)
for _ in range(100):
fa.run_one_step()
sp.run_one_step(dt=1000)
z[grid.core_nodes] += 0.001 * 1000 # Uplift
grid.imshow('topographic__elevation', cmap='terrain')Grid Types
| Grid | Use Case |
|---|---|
| Regular rectangular grids (most common) |
| Hexagonal grids (isotropic flow) |
| Irregular point distributions |
| Channel networks only |
Key Concepts
Fields and Boundaries
python
# Fields: data stored at grid elements (nodes, links, cells)
z = grid.add_zeros('topographic__elevation', at='node')
grid.at_node['drainage_area'] # Access existing field
# Boundaries: close all edges except outlet
grid.set_closed_boundaries_at_grid_edges(True, True, True, False)
z[grid.core_nodes] += uplift * dt # Core nodes exclude boundariesEssential Operations
Flow Routing
python
from landlab.components import FlowAccumulator
fa = FlowAccumulator(grid, flow_director='D8') # or 'Steepest', 'MFD'
fa.run_one_step()
drainage_area = grid.at_node['drainage_area']Stream Power Erosion
python
from landlab.components import StreamPowerEroder
sp = StreamPowerEroder(grid, K_sp=1e-5, m_sp=0.5, n_sp=1.0)
sp.run_one_step(dt=1000) # dt in yearsHillslope Diffusion
python
from landlab.components import LinearDiffuser
ld = LinearDiffuser(grid, linear_diffusivity=0.01) # m^2/yr
ld.run_one_step(dt=100)Load/Save DEM Data
python
from landlab.io import read_esri_ascii, write_esri_ascii
from landlab.io.netcdf import read_netcdf, write_netcdf
grid, z = read_esri_ascii('dem.asc', name='topographic__elevation')
write_esri_ascii('output.asc', grid, names='topographic__elevation')
write_netcdf('output.nc', grid) # Save all fieldsMulti-Component Model
python
from landlab import RasterModelGrid
from landlab.components import FlowAccumulator, StreamPowerEroder, LinearDiffuser
grid = RasterModelGrid((100, 100), xy_spacing=100.0)
z = grid.add_zeros('topographic__elevation', at='node')
z += grid.node_y / 1000 + np.random.rand(grid.number_of_nodes) * 0.1
grid.set_closed_boundaries_at_grid_edges(True, True, True, False)
fa = FlowAccumulator(grid, flow_director='D8')
sp = StreamPowerEroder(grid, K_sp=1e-5)
ld = LinearDiffuser(grid, linear_diffusivity=0.01)
dt, uplift_rate = 1000, 0.001
for _ in range(500):
fa.run_one_step()
sp.run_one_step(dt)
ld.run_one_step(dt)
z[grid.core_nodes] += uplift_rate * dtWhen to Use vs Alternatives
| Use Case | Tool | Why |
|---|---|---|
| Landscape evolution modelling | Landlab | Modular components, Python-native |
| Basin-scale stratigraphy | Badlands | Focus on sediment deposition and basin fill |
| Topographic analysis (MATLAB) | TopoToolbox | Mature MATLAB toolkit for DEM analysis |
| Simple diffusion/erosion | Custom numpy | Fewer dependencies for basic models |
| Coupled surface-subsurface | Landlab | Components for hydrology + geomorphology |
| Channel network extraction | Landlab or pysheds | Both handle flow routing well |
| Soil production and transport | Landlab | Dedicated weathering and soil components |
| Teaching geomorphology | Landlab | Clear component API, good tutorials |
Choose Landlab when: You need a modular, component-based framework for
landscape evolution modelling that combines multiple surface processes (erosion,
diffusion, flow routing, weathering) in a single simulation.
Choose Badlands when: Your focus is on basin-scale landscape evolution with
emphasis on sediment transport and stratigraphic architecture.
Choose custom numpy when: You only need a simple 2D diffusion or stream power
model without the overhead of a full component framework.
Common Workflows
Landscape Evolution Model with Erosion and Uplift
- Create with appropriate dimensions and spacing
RasterModelGrid - Initialize field (flat + noise, or load DEM)
topographic__elevation - Set boundary conditions (open one edge as outlet, close others)
- Create with chosen flow director (D8 or MFD)
FlowAccumulator - Create with erosion coefficient K_sp
StreamPowerEroder - Create for hillslope processes
LinearDiffuser - Define time step and total runtime; choose uplift rate
dt - Run time loop: flow routing, erosion, diffusion, then uplift
- Save snapshots at intervals with or
write_netcdf()write_esri_ascii() - Visualize final topography with
grid.imshow() - Analyze drainage area and channel profiles
- Extract river long profiles for steepness analysis
Common Issues
| Issue | Solution |
|---|---|
| Flat areas block flow | Add small random noise to initial topography |
| Boundary effects | Ensure at least one open boundary edge for drainage |
| Unstable erosion | Reduce |
| Wrong field name | Use exact Landlab names: |
| Memory with large grids | Reduce grid resolution or use |
Tips
- Set boundaries first - before adding components
- Use core_nodes - excludes boundary nodes for operations
- Check field names - components expect specific names (e.g., 'topographic__elevation')
- Start simple - add components incrementally and verify each
References
- Components Reference - Available components by category
- Grids Reference - Grid types and configuration
Scripts
- scripts/erosion_model.py - Basic erosion model template