Modeling the hydrological impacts of land use/land cover changes in the Andassa watershed, Blue Nile Basin, Ethiopia

被引:245
作者
Gashaw, Temesgen [1 ,3 ]
Tulu, Taffa [1 ]
Argaw, Mekuria [1 ]
Worqlul, Abeyou W. [2 ]
机构
[1] Addis Ababa Univ, Coll Nat & Computat Sci, Ctr Environm Sci, Addis Ababa, Ethiopia
[2] Texas A&M Agrilife Res, Blackland Res & Extens Ctr, Temple, TX USA
[3] Adigrat Univ, Coll Agr & Environm Sci, Dept Nat Resource Management, Adigrat, Ethiopia
关键词
Land use/land cover; CA-Markov; Hydrology; Modeling; SWAT; PLSR; LEAST-SQUARES REGRESSION; SWAT MODEL; UNCERTAINTY ANALYSIS; RIVER-BASIN; CELLULAR-AUTOMATA; SEDIMENT YIELD; SOIL-EROSION; STREAMFLOW PREDICTION; SURFACE RUNOFF; CALIBRATION;
D O I
10.1016/j.scitotenv.2017.11.191
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Understanding the hydrological response of a watershed to land use/land cover (LULC) changes is imperative for water resources management planning. The objective of this study was to analyze the hydrological impacts of LULC changes in the Andassa watershed for a period of 1985-2015 and to predict the LULC change impact on the hydrological status in year 2045. The hybrid land use classification technique for classifying Landsat images (1985, 2000 and 2015); Cellular-Automata Markov (CA-Markov) for prediction of the 2030 and 2045 LULC states; the Soil and Water Assessment Tool (SWAT) for hydrological modeling were employed in the analyses. In order to isolate the impacts of LULC changes, the LULC maps were used independently while keeping the other SWAT inputs constant. The contribution of each of the LULC classes was examined with the Partial Least Squares Regression (PLSR) model. The results showed that there was a continuous expansion of cultivated land and built-up area, and withdrawing of forest, shrubland and grassland during the 1985-2015 periods, which are expected to continue in the 2030 and 2045 periods. The LULC changes, which had occurred during the period of 1985 to 2015, had increased the annual flow (2.2%), wet seasonal flow (4.6%), surface runoff (9.3%) and water yield (2.4%). Conversely, the observed changes had reduced dry season flow (2.8%), lateral flow (5.7%), groundwater flow (7.8%) and ET (0.3%). The 2030 and 2045 LULC states are expected to further increase the annual and wet season flow, surface runoff and water yield, and reduce dry season flow, groundwater flow, lateral flow and ET. The change in hydrological components is a direct result of the significant transition from the vegetation to non-vegetation cover in the watershed. This suggests an urgent need to regulate the LULC in order to maintain the hydrological balance. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:1394 / 1408
页数:15
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