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A Comparison of Wave and Erosion Modeling Methods for the 100-Year Storm in Southern Rhode Island (3) · PREDICTING 100-YEAR STORM WAVE'S RUNUP FOR THE COAST OF RHODE ISLAND USING A FULLY NONLINEAR MODEL (3) · Aerosol pH and chemical regimes of sulfate formation in aerosol water during winter haze in the North China Plain (3) · A Conceptual Framework for Integration Development of GSFLOW Model: Concerns and Issues Identified and Addressed for Model Development Efficiency (3) · Assessing the long-term geomorphic stability of a rehabilitated landform using the CAESAR-Lisflood landscape evolution model (3) · Identifying meteorological drivers of extreme impacts: an application to simulated crop yields (3) · Keynote Speech - Modeling of Sediment Transport in the Gulf of Mexico due to the Influence of Hurricanes (3) · Implementation of runoff attenuation features into a landscape evolution model for the assessment of the impact on catchment sediment dynamics (3) · Modelling sediment storage times in alluvial floodplains (3) · The ocean and coastal response to tropical cyclone forcing in the Australian North West region (3) · Landlab: Sustainable Software Development in Practice (3) · INDIVIDUAL WAVE EFFECTS ON COASTAL STRUCTURE DAMAGE DURING WINDSTORMS (3) · Stress testing geomorphic and traditional tailings dam designs for closure using a landscape evolution model (3) · Modeling Sediment Transport Around Artificial Reefs in Southern Rhode Island (3) · High-resolution numerical weather prediction (NWP) with data assimilation over Placentia Bay, Newfoundland (3) · Shallow Flows: Research Presented at the International Symposium on Shallow Flows, Delft, Netherlands, 2003 (3) · The Effects of Ocean Surface Waves on Global Forecast in CFS Modeling System v2.0 (3) · Climatic controls on mountain glacier basal thermal regimes dictate spatial patterns of glacial erosion (3) · Ensemble Climate Projection for Hydro-Meteorological Drought over a river basin in Central Highland, Vietnam (3) · Sensitivity of Greenland ice sheet projections to spatial resolution in higher-order simulations: the AWI contribution to ISMIP6-Greenland using ISSM (3)
 
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