Management of water resources in watershed determined by avaibility accurate rainfall data. The study rationalization recorded density result the suggestion amount and placement watershed. was manage Watershed Bango with total area 246,4 km2 using Kagan-Rodda method WMO Standard. analysis Standard, 100-250 km2/rainfall shown that none existing Sub-Watershed are qualified. giving recommendation ...

Calibration of model is critical for hydrologic modeling of large watersheds in a mountain watershed. In this study Soil and Water Assessment Tool (SWAT) used to comparison a single-site calibration procedure that employed streamflow measurement at outlet of watershed to a multi-site calibration method that used streamflow measurements at three stations (Galinak, Joestan and Dehdar). Results sh...

4 Watershed modeling requires accurate estimates of precipitation, however in some cases 5 it is necessary to simulate streamflow in a watershed for which there is no precipitation gauge 6 records within close proximity to the watershed. For such cases, we propose an approach for 7 estimating watershed-scale precipitation by combining (or fusing) gauge-based precipitation 8 time series with rad...

Land cover change is a strategic issue in the Subwatershed of Danau Limau Manis. The community was triggered by big earthquake September 30, 2009, so people moved to upper watershed. problem increasing number people, damage watershed ecosystem. This can be seen from erosion river water and availability during rainy season dry season. An appropriate solution needed reduce modeling land cover. st...

CASC2D is a physically-based, distributed model that simulates the response of a watershed to precipitation. Basic processes in the model include: precipitation, interception, infiltration, surface runoff and channel flow, and erosion and deposition of upland soil and channel bed sediment. Model performance is demonstrated by applications to numerous sites such as Goodwin Creek, MS. This waters...