Sentence examples for a large watershed from inspiring English sources

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.

To that end, we exploited a database of aerial pictures to obtain classified and vectorized land uses at the field level during the past five decades of a large watershed.

This paper explores the use of three such methods, and compares their performance when used in conjunction with a lumped parameter model for surface water flow (HSPF) in 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.

This study used a large watershed, the Upper Zagunao River watershed, situated in the upper reach of the Minjiang River, the Yangtze River basin, China as an example to demonstrate how the effects of forest harvesting and climatic variability on hydrology can be quantitatively separated.

That makes good hydrological sense, since few water bodies are truly isolated and nearly all are part of a larger watershed.

Here we review the findings from the small watershed studies and present a case study of a larger watershed, the South Fork Little Red River (SFLRR) watershed (127 193 km2).

Our method was also validated by predicting mean θ of a larger watershed (Liudaogou watershed) using the θ measurement at the MTSL at Laoyemanqu watershed.

However, this approach requires an effective information system that can process both the characteristics of the river basin and the agricultural activities using at least two embedded scales: the scale of the small agricultural catchment for action by farmers and the scale of a larger watershed for public decision making.

Although these studies were conducted in small spring watersheds that were not subject to flooding, the contributions of these changes to the spring flow in a larger watershed comprising many of these degraded springs could lead to a significant intensification of flood hazards.