Geomorphic modeling aims to use mathematical and computational techniques to simulate and predict how landscapes will evolve over time.

Channel migration models are specifically designed to simulate the lateral movement of river channels and the formation of meanders.

The resolution of a DEM is the size of each pixel, which determines the level of detail in the elevation data.

Cellular automata modeling is a grid-based approach where each cell represents a small portion of the landscape and its state changes over time based on the states of neighboring cells.

Erosion is the primary driving force behind landscape evolution in most geomorphic models, as it sculpts and modifies the land surface.

Sediment transport models are specifically designed to simulate the transport and deposition of sediment by water, wind, or ice.

The timestep in a geomorphic model is the interval at which the model is updated and the landscape is modified.

Coastal evolution models are specifically designed to simulate the interactions between coastal landforms, sea-level change, and sediment transport.

Calibration is the process of adjusting the parameters of a geomorphic model to ensure that it accurately reproduces observed landscape features or processes.

Ice sheet models are specifically designed to simulate the dynamics of ice sheets, including their growth, retreat, and interactions with the underlying bedrock.

Uncertainty analysis is the process of assessing the range of possible outcomes of a geomorphic model and identifying the factors that contribute to uncertainty.

Hillslope evolution models are specifically designed to simulate the processes that shape hillslopes, including soil erosion, deposition, and the formation of landforms such as gullies and landslides.

Verification is the process of testing a geomorphic model against observed data to assess its accuracy and ability to reproduce real-world landscape features or processes.

Delta evolution models are specifically designed to simulate the formation and evolution of river deltas, including the interactions between fluvial sediment transport and marine processes such as waves and tides.

Sensitivity analysis is the process of identifying the most influential parameters in a geomorphic model and assessing their impact on the model's predictions.