Assimilating Soil Moisture Information to Improve the Performance of SWAT Hydrological Model

被引:3
|
作者
Kofidou, Maria [1 ]
Gemitzi, Alexandra [1 ]
机构
[1] Democritus Univ Thrace, Fac Engn, Dept Environm Engn, V Sofias 12, Xanthi 67100, Greece
关键词
hydrological modeling; SMAP; soil moisture; SWAT-CUP; Vosvozis River Basin; CATCHMENT SCALE; CALIBRATION; VALIDATION; SYSTEM; EUROPEEN; CLIMATE; BASIN; SHE;
D O I
10.3390/hydrology10080176
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
The present work aims to highlight the possibility of improving model performance by assimilating soil moisture information in the calibration and validation process. The Soil and Water Assessment Tool (SWAT) within QGIS, i.e., QSWAT, was used to simulate the hydrological processes within the test basin, i.e., Vosvozis River Basin (VRB) in NE Greece. The model calibration and validation were conducted via SWAT-CUP for a four-year period from 2019 to 2022, in three different ways, i.e., using the traditional calibration process with river flow measurements, using satellite-based soil moisture only in the calibration, and finally incorporating satellite-based soil moisture datasets and calibrating using simultaneously flow and soil moisture information. All modeling approaches used the same set of input data related to topography, land cover, and soil information. This study utilized the recently released global scale daily downscaled soil moisture at 1 km from the Soil Moisture Active Passive (SMAP) mission to generate soil moisture datasets. Two performance indicators were evaluated: Nash Sutcliffe (NS) and coefficient of determination (R-2). Results showed that QSWAT successfully simulated river flow in VRB with NS = 0.61 and R-2 = 0.69 for the calibration process using river flow measurements at the outlet of VRB. However, comparing satellite-based soil moisture, NS and R-2 were considerably lower with an average derived from the 19 subbasins (NS = 0.55, R-2 = 0.66), indicating lower performance related to the simulation of soil moisture regime. Subsequently, introducing satellite-derived soil moisture as an additional parameter in the calibration process along with flow improved the acquired average soil moisture results of the 19 subbasins (NS = 0.85, R-2 = 0.91), while preserving the satisfactory performance related to flow simulation (NS = 0.57, R-2 = 0.66). Our work thus demonstrates how assimilating available satellite-derived soil moisture information into the SWAT model may offer considerable improvement in the description of soil moisture conditions, keeping the satisfactory performance in flow simulation.
引用
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页数:33
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