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List of results

• A mesh independent flow direction model for hydrologic models  +
• A method to test for order in a vertical succession of strata  +
• A model of dunes and snow-waves  +
• A set of Matlab functions for topographic analysis  +
• A simple kinematic model of meandering  +
• A simple parallel code to demonstrate diffusion  +
• A simple snow model  +
• A spatially explicit model of coastal barrier evolution  +
• A zone-based taxon  +
• Aeolian dune landscape model  +
• Aggregate scale morphodynamic model of integrated coastal systems  +
• Alaskan Frame‐based Ecosystem Code  +
• Alluvial morphodynamics of bedrock reaches  +
• Barrier Island Translation model  +
• Barrier-Bay-Marsh-Forest Transect Coupled Model Framework  +
• Basin and landscape dynamics  +
• Basin filling stratigraphic model  +
• Bed-material sediment transport and storage dynamics on river networks.  +
• Bedload transport model  +
• Bergen Ocean Model  +
• Biogenic mixing of marine sediments  +
• Build and destroy strath and fill terraces  +
• Calculate Chi Indices  +
• Calculate Hack parameters.  +
• Calculate steepness and concavity indices from gridded topography  +
• A model representing infiltration, interception, and runoff using the kinematic wave approximation  +
• A multi-dimensional Eulerian two-phase model for sediment transport (version 2.0)  +
• A numerical method to analyse a vertical succession of strata and identify the most cyclical arrangement of constituent facies  +
• A probabilistic sediment cascade model for sediment production, storage and transfer  +
• A set of MATLAB functions to model how luminescence evolves in different geomorphic scenarios.  +
• A stand alone model for the morphological evolution of an idealized transect across a marsh channel-and-platform.  +
• A state-of-the-art finite-element computer simulation program for coastal ocean circulation modeling  +
• A suite of Digital Elevation Model (DEM) tools for the extraction and analysis of hydrologic information from topography as represented by a DEM. TauDEM 5 is a new version implemented to take advantage of parallel processing  +
• A turbulence-resolving numerical model for fine sediment transport in bottom boundary layer  +
• A turbulent boundary layer model for the linearized shallow water equations  +
• ANUGA is a hydrodynamic modelling tool that allows users to model realistic flow problems in complex 2D geometries.  +
• Add-on package to ANUGA with modules for sediment transport and vegetation drag  +
• AeoLiS is a process-based model for simulating aeolian sediment transport in situations where supply-limiting factors are important, like in coastal environments.  +
• Algorithm for directly measuring hillslope length from high resolution topographic data  +
• Algorithm for extracting channel networks from high resolution topographic data  +
• An easy-to-use MATLAB code to simulate long-term lithosphere and mantle deformation.  +
• An iceberg drift and melt model, developed to simulate sedimentation in high-latitude glaciated fjords.  +
• An immersed boundary, Navier–Stokes code for the simulation of gravity and turbidity currents interacting with complex topographies.  +
• An implementation of the Implicit Drainage Area method (regular and hybrid versions) for calculating drainage area from flow directions using parallel iterative solvers.  +
• An intermediate complexity model for simulating stream channel evolution (years to decades) at the watershed scale.  +
• An updated Lagrangian explicit finite difference code for modeling a finitely deforming elasto-visco-plastic solid in 3D.  +
• Analysis of time-variable gravity from the GRACE satellite mission using spherical harmonics and spherical Slepian functions  +
• BlockLab computes landscape evolution in the presence of large blocks of rock on hillslopes and in channels.  +
• COAWST: A Coupled-Ocean-Atmosphere-Wave-Sediment Transport Modeling System  +
• Caesar Lisflood is a morphodynamic / Landscape evolution model that simulates erosion and deposition in river catchments and reaches over time scales from hours to 1000's of years.  +