River flow decline across the entire Arkansas River Basin in the 21st century

被引:4
|
作者
Yang, Jia [1 ,6 ]
Zou, Chris [1 ]
Will, Rodney [1 ]
Wagner, Kevin [2 ]
Ouyang, Ying [3 ]
King, Chad [4 ]
Winrich, Abigail [1 ]
Tian, Hanqin [5 ]
机构
[1] Oklahoma State Univ, Dept Nat Resource Ecol & Management, Div Agr Sci & Nat Resources, Stillwater, OK 74078 USA
[2] Oklahoma State Univ, Oklahoma Water Resources Ctr, Div Agr Sci & Nat Resources, Stillwater, OK 74078 USA
[3] Ctr Bottomland Hardwoods Res, USDA Forest Serv, 775 Stone Blvd, Thompson Hall, Room 309, Mississippi, MS 39762 USA
[4] Univ Cent Oklahoma, Dept Biol, 100 N Univ Dr, Edmond, OK 73034 USA
[5] Boston Coll, Schiller Inst Integrated Sci, Dept Earth & Environm Sci & Soc, Chestnut Hill, MA 02467 USA
[6] Oklahoma State Univ, Dept Nat Resource Ecol & Management, 008 Ag Hall, Stillwater, OK 74078 USA
关键词
Climate change; Hydrological modeling; Droughts; Surface runoff; Great plains; Evapotranspiration; GLOBAL TERRESTRIAL EVAPOTRANSPIRATION; LAND-COVER CHANGE; CLIMATE-CHANGE; MISSISSIPPI RIVER; MANN-KENDALL; RISING CO2; WATER; IRRIGATION; DROUGHT; RUNOFF;
D O I
10.1016/j.jhydrol.2023.129253
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The Arkansas River and its tributaries provide critical water resources for agricultural irrigation, hydropower generation, and public water supply in the Arkansas River Basin (ARB). However, climate change and other environmental factors have imposed significant impacts on regional hydrological processes, resulting in wide-spread ecological and economic consequences. In this study, we projected future river flow patterns in the 21st century across the entire ARB under two climate and socio-economic change scenarios (i.e., SSP2-RCP45 and SSP5-RCP85) using the process-based Dynamic Land Ecosystem Model (DLEM). We designed "baseline simula-tions" (all driving factors were kept constant at the level circa 2000) and "environmental change simulations" (at least one driving factor changed over time during 2001-2099) to simulate the inter-annual variations of river flow and quantify the contributions of four driving factors (i.e., climate change, CO2 concentration, atmospheric nitrogen deposition, and land use change). Results showed that the Arkansas River flow in 2080-2099 would decrease by 12.1% in the SSP2-RCP45 and 27.9% in the SSP5-RCP85 compared to that during 2000-2019. River flow decline would occur from the beginning to the middle of this century in the SSP2-RCP45 and happen throughout the entire century in the SSP5-RCP85. All major rivers in the ARB would experience river flow decline with the largest percentage reduction in the western and southwestern ARB. Warming and drying cli-mates would account for 77%-95% of the reduction. The rising CO2 concentration would exacerbate the decline through increasing foliage area and ecosystem evapotranspiration. This study provides insight into the spatial patterns of future changes in water availability in the ARB and the underlying mechanisms controlling these changes. This information is critical for designing watershed-specific management strategies to maintain regional water resource sustainability and mitigate the adverse impacts of climate changes on water availability.
引用
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页数:16
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