Discharge data have been collected for over 40 years and are maintained by the Bangladesh Water Development Board. These data are of high quality and frequently used in calibration and validation
of the basinwide hydrological models (Gain et al., 2011, Immerzeel, 2008 and Jian et al., 2009). In addition to weather information, SWAT requires soil properties and land cover information to simulate loads in the hydrological components. The soil map was obtained from the Food and Agriculture Organization of the United Nations (FAO, 1995). R428 At a spatial resolution of 10 km, 106 soil types for the Brahmaputra basin were differentiated, and soil properties for two layers (0–30 cm and 30–100 cm depth) were provided. Other soil properties such as particle-size distribution, bulk density, organic carbon content, check details available water capacity, and saturated hydraulic conductivity were obtained from Reynolds
et al. (1999). The land use and land cover map was obtained from the U.S. Geological Survey (USGS) Global Land Cover Characterization database version 2.0 at 1000 m spatial resolution (Loveland et al., 2000). The original 24 categories were reclassified into 12 to match the land use database of SWAT. Both the soil and land use and land cover maps were resampled to 180 m to correspond to the spatial resolution of the digital elevation model (DEM) used in the simulations. The geographic information system interface – ArcSWAT (Winchell et al., 2010) – was used to parameterize the model for the Brahmaputra basin. The stream network of the basin was delineated from a 180-m DEM resampled from the HydroSHEDS (Hydrological
data and maps based on Shuttle Elevation Derivatives at multiple scales) dataset (Lehner et al., 2008). Montelukast Sodium Requiring a minimum drainage area of 12,000 km2 and including an additional outlet at Bahadurabad discharge gauge station, the basin was subdivided into 29 subbasins. The outlet at the Bahadurabad discharge station constitutes a drainage area of 519,408 km2. The outlet at Bahadurabad station was considered to be the final outlet of the Brahmaputra basin (Fig. 1). Characterization of the stream reaches and subbasin geomorphology was done automatically by the interface. To further characterize the subbasin for dominant land use and soil types, the multiple Hydrological Response Unit (HRU) option in SWAT was implemented, which resulted in discretization of 527 HRUs for the Brahmaputra basin. The Brahmaputra is a large basin with diverse elevations. Changes in elevation within the basin strongly influence the snow accumulation and melt process (Pomeroy and Brun, 2001), which can be simulated better when elevation bands and their corresponding subbasin area fractions are defined (Fontaine et al., 2002). To account for the basin’s elevation gradient for snow accumulation and melt processes, 10 elevation bands were incorporated at 500-m increments for the maximum allowable range of 2393–6719 m.