PREDICTION OF FUTURE WATER QUALITY UNDER LONG-TERM CLIMATE CHANGE IN URAYAMA RESERVOIR

Q4 Environmental Science
Jungkyu Choi, H. Yajima, K. Taniguchi, J. Magome
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引用次数: 1

Abstract

A 3-D coupled hydrodynamic and ecological model of ELCOM-CAEDYM was applied to Urayama Reservoir to study the effects of climate change on the thermal structure and water quality in the reservoir as well as those downstream. We evaluated the differences between present period (2002-2010) and future period (2062-2070). Scenarios were estimated using JRA25 and GFDL-CM3 with CO 2 emission scenario of RCP4.5 by downscaling of WRF model and a hydrological model of YHyM/BTOPMC. Future surface and hypolimnetic water temperatures were predicted to rise by 2.9°C and 1.6°C, respectively. As a result, a stronger thermal stratification was expected. In the reservoir, significant increase of future SS concentrations by more frequent and bigger floods and decrease of phytoplankton biomasses by high water temperature, hydrologic condition and light limitation were also predicted. In the downstream of the reservoir, less frequent cold-water release and more frequent warm-water release were both predicted. Moreover, more frequent and high turbid water releases were predicted due to more frequent and bigger floods in the future.
长期气候变化下村山水库未来水质预测
将ELCOM-CAEDYM三维水动力与生态耦合模型应用于浦山水库,研究气候变化对库区及下游热结构和水质的影响。我们评估了当期(2002-2010)和未来期(2062-2070)之间的差异。通过WRF模型和YHyM/BTOPMC水文模型的降尺度,利用JRA25和GFDL-CM3估算了RCP4.5 co2排放情景。预计未来地表水温和低表层水温将分别上升2.9°C和1.6°C。因此,预计会有更强的热分层。未来水库内SS浓度将因更频繁和更大的洪水而显著增加,而高水温、水文条件和光照限制将导致浮游植物生物量减少。在水库下游,冷水释放频率较低,温水释放频率较高。此外,由于未来洪水更频繁、更大,预计浑浊水释放频率更高。
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来源期刊
Journal of Japan Society of Civil Engineers
Journal of Japan Society of Civil Engineers Environmental Science-Environmental Engineering
CiteScore
0.60
自引率
0.00%
发文量
34
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