Large area water resources development and management require an understanding of basic hydrologic processes and simulation capabilities at the river basin scale. We define large areas as river basins of thousands or tens of thousands of square kilometers. Current concerns that are motivating the development of large area hydrologic modeling include climate change, management of water supplies in arid regions, large scale flooding, and offsite impacts of land management. Recent advances in computer hardware and software including increased speed and storage, advanced software debugging tools, and GIS/spatial analysis software have allowed large area simulation to become feasible. The objective of this overview is to briefly describe the history, an overview of model operation, and a description of model components of a river basin scale model called SWAT (Soil and Water Assessment Tool). SWAT is the continuation of a long-term effort of nonpoint source pollution modeling with the USDA-Agricultural Research Service (ARS). In the early to mid-1970's, in response to the Clean Water Act, ARS assembled a team of interdisciplinary scientists from across the U.S. to develop a process-based, nonpoint source simulation model. From that effort, a model called CREAMS (Chemicals, Runoff, and Erosion from Agricultural Management Systems) was developed (Knisel, 1980). CREAMS is a field scale model developed to simulate the impact of land management on water, sediment, nutrients, and pesticides leaving the edge of a field. By the early and mid-1980's, several models were being developed with origins from the original CREAMS model. GLEAMS (Groundwater Loading Effects on Agricultural Management Systems) (Leonard et al., 1987) concentrated on pesticide and nutrient groundwater loadings. A model called EPIC (Erosion-Productivity Impact Calculator) (Williams et al., 1985) was originally developed to simulate the impact of erosion on crop productivity and has now evolved into a comprehensive agricultural management, field scale, nonpoint source loading model. Other efforts involved modifying CREAMS to simulate complex watersheds with varying soils, land use, and management. One effort was the AGNPS (Agricultural Nonpoint Source) (Young et al., 1987) model. AGNPS is a spatially detailed, single event (storm) model that subdivides complex watersheds into grid cells. A model called SWRRB (Simulator for Water Resources in Rural Basins) (Williams et al., 1985; Arnold et al., 1990) was developed to simulate nonpoint source loadings from watersheds. SWRRB is a continuous time (daily time step model) that allows a basin to be subdivided into a maximum of ten subbasins. To create SWRBB, the CREAMS daily rainfally hydrology model was modified for application to large, complex, rural basins. The major changes involved were (a) the model was expanded to allow simultaneous computations on several subbasins to predict the basin water yield; (b) a return flow component was added; (c) a reservoir storage component was added for use in determining the effects of farm ponds and reservoirs on water and sediment yield; (d) a weather simulation model (rainfall, solar radiation, and temperature) was added to provide for longer-term simulations and more representative weather inputs, both temporally and spatially; (e) a better method was developed for predicting the peak runoff rate; (f) a crop growth model was added to account for annual variation in growth; (g) a simple flood routing component was added; (h) components were added to simulate sediment movement through ponds, reservoirs, streams, and valleys; and (i) transmission losses were calculated. In the late 1980's, most of the SWRRB model development has been focused on problems involving water quality. Example additions include the GLEAMS (Leonard et al., 1987) pesticide fate component, optional SCS technology for estimating peak runoff rates, and newly developed sediment yield equations. These and other less significant developments extended SWRRB's capabilities to deal with a wide variety of watershed management problems. Also in the late 1980's, the Bureau of Indian Affairs needed a model to estimate the downstream impact of water management within Indian reservation lands in Arizona and New Mexico. SWRRB was utilized for smaller watersheds within the basin (up to a few hundred square kilometers), but it was necessary to simulate streamflow from much larger basins (several thousand square kilometers). This required the basin to be divided into several hundred subwatersheds. SWRRB was limited to ten subbasins and also had a simplistic routing structure with outputs routed from the subbasin outlets directly to the basin outlet. This problem led to the development of a model called ROTO (Routing Outputs to Outlet) (Arnold et al., 1995). ROTO was developed to take output from multiple SWRRB runs and route the flows through channels and reservoirs. ROTO provided a reach routing approach and overcame the SWRRB subbasin limitation by "linking" multiple SWRRB runs together. Although this approach was effective, the input and output of multiple SWRRB output files was cumbersome and required considerable computer storage. Limitations also occurred because all SWRRB runs had to be made independently, and then input to ROTO for the channel and reservoir routing. Thus, the SWAT model was developed by merging SWRRB and ROTO into one basin scale model. SWAT allows a basin to be divided into hundreds or thousands of grid cells or subwatersheds. SWAT is still a continuous time model (daily time step) that is required to look at long-term impacts of management (i.e., reservoir sedimentation over 50-100 years) and also timing of agricultural practices within a year (i.e., crop rotations, planting and harvest dates, irrigation, fertilizer, and pesticide application rates and timing). MODEL OPERATION SWAT is a continuous time model that operates on a daily time step. The objective in model development was to predict the impact of management on water, sediment and agricultural chemical yields in large ungaged basins. To satisfy the objective, the model (a) is physically based (calibration is not possible on ungaged basins); (b) uses readily available inputs; (c) is computationally efficient to operate on large basins in a reasonable time, and (d) is continuous time and capable of simulating long periods for computing the effects of management changes. SWAT uses a command structure for routing runoff and chemicals through a watershed similar to the structure of HYMO (Williams and Hann, 1973). Commands are included for routing flows through streams and reservoirs, adding flows, and inputting measured data or point sources. Using a routing command language, the model can simulate a basin subdivided into grid cells or subwatersheds. Additional commands have been developed to allow measured and point source data to be input to the model and routed with simulated flows. Also, output data from other simulation models can be input to SWAT. Using the transfer command, water can be transferred from any reach or reservoir to any other reach or reservoir within the basin. The user can specify the fraction of flow to divert, the minimum flow remaining in the channel or reservoir, or a daily amount to divert. The user can also apply water directly to a subbasin for irrigation. Although the model operates on a daily time step and is efficient enough to run for many years, it is intended as a long term yield model and is not capable of detailed, single-event, flood routing.