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Relating Design Storm Events to Ordinary High Water Marks in Indiana

机译:将设计风暴事件与印第安纳州的普通高水位线相关

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摘要

Hydraulic design and environmental permitting are heavily dependent upon Ordinary High Water Marks (OHWM) because they define the active river channel. The United States Army Corps of Engineers (USACE) use OHWM for regulation of the “Waters of the United States” as well as for flood and drought management. Current methods to determine OHWM are based on detailed on-site surveys to identify physical characteristics like scouring, deposition around the banks, absence of vegetation and water staining. These characteristics are site specific so there are fluctuations in measurements based on the water body, weather conditions, channel morphology, slope, fluvial patterns and size of the channel. A more reliable way to estimate this variable for hydraulic design is required that is based on storm return periods. This study uses hydrologic and hydraulic modeling to relate OHWM to storm return periods by analyzing hydraulic and hydrologic parameters corresponding to design streamflow events for 26 watersheds in Indiana. The results show that the OHWM corresponds to discharges that have return periods ranging from 0.7 – 1.1 years. These results also suggest that that OHWM correspond to channel discharges much smaller than bank-full discharge, which typically has a return period of 1.5 – 2 years. The OHWM discharges are then related to 100-year discharges to enable the use of this relationship in approximately estimating the OHWM discharge when the 100-year discharge is known. For Indiana, it is found that ratio of OHWM discharge and 100-year discharge has an average value of 4.99% for the northern part, 3.60% for the central part, and 5.49% for the southern part.
机译:水力设计和环境许可在很大程度上取决于普通高水位线(OHWM),因为它们定义了活动河道。美国陆军工程兵团(USACE)使用OHWM来管理“美国水域”以及洪水和干旱管理。当前确定OHWM的方法是基于详细的现场调查,以识别物理特征,如擦洗,河岸附近沉积,没有植被和水渍。这些特征是特定于地点的,因此,根据水体,天气状况,河道形态,坡度,河床样式和河道大小,测量值会有波动。需要一种更可靠的方法来估算水力设计的变量,该方法基于暴风雨回潮期。这项研究通过分析与印第安纳州26个流域的设计水流事件相对应的水力和水文参数,利用水文和水力模型将OHWM与暴风雨的重现期联系起来。结果表明,OHWM对应的回收期为0.7 – 1.1年。这些结果还表明,OHWM对应的通道放电要比全流放电小得多,后者通常具有1.5 – 2年的恢复期。然后,将OHWM排放与100年排放相关联,以便在已知100年排放时大致估计OHWM排放时可以使用此关系。对于印第安纳州,发现OHWM排放量与100年排放量之比的平均值在北部为4.99%,中部为3.60%,南部为5.49%。

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