Hydrological Modeling of Climate Change Impacts in a Tropical River Basin: A Case Study of the Cauto River, Cuba

被引:13
|
作者
Montecelos-Zamora, Yalina [1 ]
Cavazos, Tereza [2 ]
Kretzschmar, Thomas [1 ]
Vivoni, Enrique R. [3 ,4 ]
Corzo, Gerald [5 ]
Molina-Navarro, Eugenio [6 ]
机构
[1] CICESE, Dept Geol, Ensenada 22860, Baja California, Mexico
[2] CICESE, Dept Oceanog Fis, Ensenada 22860, Baja California, Mexico
[3] Arizona State Univ, Sch Earth & Space Explorat, Tempe, AZ 85287 USA
[4] Arizona State Univ, Sch Sustainable Engn & Built Environm, Tempe, AZ 85287 USA
[5] UNESCO IHE Inst Water Educ, Dept Integrated Water Syst & Governance, NL-2611 Delft, Netherlands
[6] Aarhus Univ, Dept Biosci, DK-8600 Silkeborg, Denmark
关键词
rainfall-runoff modeling; SWAT; RegCM4; 3; Cuba; climate change; water management; LAND-USE CHANGE; WATER-BALANCE; PARAMETER SENSITIVITY; SWAT; CALIBRATION; STREAMFLOW; CATCHMENT; PRECIPITATION; ENCROACHMENT; TEMPERATURE;
D O I
10.3390/w10091135
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The soil and water assessment tool (SWAT) model was applied for the first time in Cuba to assess the potential impacts of climate change on water availability in the Cauto River basin. The model was calibrated (and validated) for the 2001-2006 (2007-2010) period at a monthly timescale in two subbasins La Fuente and Las Coloradas, representative of middle and upper sections of the Cauto basin; the calibrated models showed good performance. The output available for the regional climate Model RegCM4.3 was used to force the calibrated SWAT models to simulate a baseline (1970-2000) period and near-future (2015-2039) hydrologic regimes under the representative concentration pathway (RCP) 8.5 emission scenario. The future projections suggest regional increases of 1.5 degrees C in mean annual temperature and a 38% decrease in mean annual precipitation in the subbasins. These changes translate to possible reductions in the annual streamflow of up to 61% with respect to the baseline period, whereas the aquifer recharge in the basin is expected to decrease up to 58%, with a consequent reduction of groundwater flow, especially during the boreal summer wet season. These projection scenarios should be of interest to water resources managers in tropical regions.
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页数:25
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