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MODIFICATION OF DWCM-AGWU MODEL APPLIED TO A PADDY-DOMINANT BASIN WITH LARGE DAMS

机译:DWCM-AGWU模型在大面积稻田上的应用

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The DWCM-AgWU (Distributed Water Circulation Model incorporating Agricultural Water Use)model was modifi ed and applied to assess the water use in the Chao Phraya River basinof the years 2008–2011, which included both droughts and fl oods. A cooperating reservoirmanagement model was introduced to incorporate two large dams, the Bhumibol and SirikitDams with several remote irrigated areas in water allocation/management. Besides, specialtreatment of fl ood peaks was also added to take agricultural practices into consideration.The two large dams are the main sources of irrigation water during dry seasons and they arealso responsible for controlling fl oods in the downstream during rainy seasons. For the lowerreaches of the Basin from Nakhon Sawan to the sea, another special water management inrainy days when the release at the Chao Phraya diversion Dam was controlled at a thresholdwas applied. As a result of the simulation, the average relative error between the calculatedand observed daily fl ow volume was 20.1% at the station of Nakhon Sawan, which is locatedbelow the convergence of the four basins of the main tributaries of the Chao Phraya River and37.1% at the downstream point of the Chao Phraya diversion Dam below intake facilities whichsupply irrigated water to the project. Then, modifi ed model will enable continuous calculationsfor mitigating the impacts of extreme events such as the 2011 fl ood in Thailand, for managingthe use of irrigation water, and for proposing adaptive countermeasures to climate change.
机译:DWCM-AgWU(结合农业用水的分布式水循环模型) 修改模型并将其用于评估湄南河流域的用水 2008-2011年,包括干旱和洪水。合作水库 引入了管理模型,以合并两个大型水坝:普密蓬和诗丽吉 在水的分配/管理中有几个偏远灌溉区的水坝。此外,特别 还增加了对洪峰的处理,以考虑到农业实践。 这两个大水坝是旱季灌溉水的主要来源,它们是 还负责控制雨季下游的洪水。对于较低 从那空沙旺到海域的流域,另一种特殊的水管理 雨天,湄南河引水坝的释放被控制在一个阈值 已应用。作为仿真结果,计算出的平均相对误差为 在位于那空沙旺(Nakhon Sawan)站的每日流量观测值为20.1% 在湄南河主要支流的四个盆地的汇合处和 湄南河引水坝下游进水口以下37.1% 为项目供应灌溉水。然后,修改后的模型将使连续计算成为可能 用于减轻极端事件(例如泰国2011年洪水)的影响, 灌溉用水的使用,以及提出应对气候变化的对策。

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