二维数值模拟在2014年2月玻利维亚亚马逊河流域洪水分析中的应用——新HEC-RAS版本5的应用

IF 0.2 Q4 WATER RESOURCES RIBAGUA-Revista Iberoamericana del Agua Pub Date : 2016-01-01 DOI:10.1016/j.riba.2015.12.001
V. Moya Quiroga , S. Kure , K. Udo , A. Mano
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引用次数: 176

摘要

莫克斯大平原是玻利维亚亚马逊地区的广阔平原,不断被马莫雷河淹没。洪水持续数天,影响了特立尼达等重要城市,淹没了人民、牲畜和可耕地。由于多云的天气,遥感观测仅限于部分地区和几天。因此,洪水事件的特征和可能的后果存在巨大的不确定性。二维数值模拟已被证明是了解洪水事件的重要工具。HEC-RAS模型是最流行的水力模型之一。2014年,新版本的HEC-RAS (HEC-RAS-v5)发布,包括2D功能。本研究应用新的HEC-RAS-v5模拟了2014年2月玻利维亚亚马逊地区的洪水事件。将模拟的洪水与卫星图像进行对比,结果表明模拟效果良好。此外,模拟还提供了诸如水深、流速和洪水的时间变化等信息。确定了水开始溢出的具体位置。在大部分淹水区域,水流速度低于0.25 m s−1。在洪水的前十天,洪水范围迅速增加。通过洪水深度可以确定不同危险程度的地区。Mamore河的西部平原是最容易受到洪水侵袭的地区;洪水范围大,持续时间长,水深深。威胁特立尼达城市的洪水起源于两个地方;一个位于北部32公里处,另一个位于西南10公里处。来自北部的洪水在开始泛滥12天后接近特立尼达,而来自南部的洪水在开始泛滥7天后接近特立尼达。虽然来自北方的洪水比来自南方的洪水更深,但来自南方的洪水在北方之前开始泛滥。因此,水媒和病媒传播的疾病可能在南方比北方更早发源于南方。洪水开始泛滥五天后,圣哈维尔市被洪水淹没。研究显示了新的HEC-RAS在洪水研究中的适用性和二维能力的价值。
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Application of 2D numerical simulation for the analysis of the February 2014 Bolivian Amazonia flood: Application of the new HEC-RAS version 5

Llanos de Moxos are vast plains in the Bolivian Amazonia that are continually flooded by the Mamore river. The flood lasts for several days affecting important cities like Trinidad, drowning people, drowning cattle and swamping arable land. Because of the cloudy skies, remote sensing observations are limited to some areas and few days. Thus, there is huge uncertainty about characteristics of flood events and possible consequences. Two-dimensional (2D) numerical simulation proved to be an important tool for understanding flood events. The HEC-RAS model is one of the most popular hydraulic models. In 2014 a new version of HEC-RAS (HEC-RAS-v5) was released including 2D capabilities. The present study applied the new HEC-RAS-v5 to simulate the February 2014 flood event in the Bolivian Amazonia. The flood simulated shows good performance when compared with satellite image of the flood event. In addition, the simulation provides information like water depth, flow velocity and a temporal variation of the flood. Specific locations where water begins to overflow were identified. Over most of the flooded area the water velocity is lower than 0.25 m s−1. During first ten days of the flood the flood extent increases rapidly. The flood depth allows identifying areas exposed to different hazard levels. The west plain of the Mamore river is the most exposed to the flood; it shows bigger flood extent, longer flood duration and deeper water depth. The flood that threatens the city of Trinidad originates in two locations; one located 32 km at the north and other located 10 km at the south west. The flood from the north gets close to Trinidad twelve days after it begins to overflow, while the flood from the south gets close to Trinidad seven days after it begins to overflow. Although the flood from the north is deeper than the flood from the south, the flood from the south begins flooded before the north. Thus, water borne and vector borne diseases may originate at the south earlier than the north. The city of San Javier gets covered by flood five days after the water begins to overflow. The study shows the applicability and the value of the 2D capabilities of the new HEC-RAS for flood studies.

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