4.6 Article

Development of Web-Based RECESS Model for Estimating Baseflow Using SWAT

Journal

SUSTAINABILITY
Volume 6, Issue 4, Pages 2357-2378

Publisher

MDPI
DOI: 10.3390/su6042357

Keywords

baseflow; integrated river basin management; web-based RECESS; recession; SWAT; alpha factor

Funding

  1. Geo-Advanced Innovative Action (GAIA) Project in Republic of Korea [RE201402074]
  2. Korea Environmental Industry & Technology Institute (KEITI) [ARQ201402057001] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)

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Groundwater has received increasing attention as an important strategic water resource for adaptation to climate change. In this regard, the separation of baseflow from streamflow and the analysis of recession curves make a significant contribution to integrated river basin management. The United States Geological Survey (USGS) RECESS model adopting the master-recession curve (MRC) method can enhance the accuracy with which baseflow may be separated from streamflow, compared to other baseflow-separation schemes that are more limited in their ability to reflect various watershed/aquifer characteristics. The RECESS model has been widely used for the analysis of hydrographs, but the applications using RECESS were only available through Microsoft-Disk Operating System (MS-DOS). Thus, this study aims to develop a web-based RECESS model for easy separation of baseflow from streamflow, with easy applications for ungauged regions. RECESS on the web derived the alpha factor, which is a baseflow recession constant in the Soil Water Assessment Tool (SWAT), and this variable was provided to SWAT as the input. The results showed that the alpha factor estimated from the web-based RECESS model improved the predictions of streamflow and recession. Furthermore, these findings showed that the baseflow characteristics of the ungauged watersheds were influenced by the land use and slope angle of watersheds, as well as by precipitation and streamflow.

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