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Sediment output from a post-mining catchment – Centennial impacts using stochastically generated rainfall (3) · How to account for particle size effects in a landscape evolution model when there is a wide range of particle sizes (3) · The Regional Ocean Modeling System (ROMS) 4-dimensional variational data assimilation systems (3) · A Coupled Atmosphere–Wave–Ocean Modeling System: Simulation of the Intensity of an Idealized Tropical Cyclone (3) · Soil erosion predictions from a landscape evolution model – An assessment of a post-mining landform using spatial climate change analogues (3) · Modeling sediment movement and channel response to rainfall variability after a major earthquake (3) · Modelling the impact of seismic triggered landslide location on basin sediment yield, dynamics and connectivity (3) · Bayeslands: A Bayesian inference approach for parameter uncertainty quantification in Badlands (3) · Understanding post-mining landforms: Utilising pre-mine geomorphology to improve rehabilitation outcomes (3) · Rainfall spatial-heterogeneity accelerates landscape evolution processes (3) · Coastal Erosion Management by Implementing Concept of Building with Nature (BwN) in Demak Regency, Central Java, Indonesia (3) · Assessing climate change impacts on the stability of small tidal inlets: Part 2 - Data rich environments (3) · SedFoam: A multi-dimensional Eulerian two-phase model for sediment transport and its application to momentary bed failure (3) · Three-dimensional scour simulations with a two-phase flow model (3) · Simulating tidal and storm surge hydraulics with a simple 2D inertia based model, in the Humber Estuary, U.K (3) · Landscape evolution of the Wenchuan earthquake-stricken area in response to future climate change (3) · Modelling headwater channel response and suspended sediment yield to in-channel large wood using the Caesar-Lisflood landscape evolution model (3) · Impacts of Seagrass Dynamics on the Coupled Long‐Term Evolution of Barrier‐Marsh‐Bay Systems (3) · Catchment reconstruction — erosional stability at millennial time scales using landscape evolution models (3)
 
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