Exact(37)
In large watersheds longer hydrological forecasts are possible.
Nevertheless, these effects have not been adequately documented in large watersheds >10,000 ha.
However, separating their relative contributions to hydrology is rarely examined, particularly in large watersheds (>1000 km2).
L can be calculated for large watersheds using the unit contributing area (UCA) or the slope length as input parameters.
Likewise, the techniques employed may find useful applications for water resources management at the scale of large watersheds.
Uncalibrated model simulations show broad underestimation of flood peaks for small watersheds and overestimation those for large watersheds.
Similar(23)
The Little Colorado River which drains the Mogollon Rim's lee side and flows from southeast to northwest into the Colorado River between Marble Canyon and the Grand Canyon draws and transports little water from its large watershed.
This should allow more realistic appraisal of various land use management practices on a large watershed.
This approach can upscale model prediction for a small watershed with the calibrated SWAT model to a large watershed, generating spatial and temporal estimations of groundwater recharge and nitrate loading for the large watershed.
In this paper, we focus on the impact of spatial rainfall variability on H/NPS modeling of a large watershed.
This article introduces an integrated washland optimization model that is developed to evaluate flood mitigation alternatives by installation of washlands in a large watershed.
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