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Validation of the NOS Galveston Bay Nowcast/Forecast SystemHydrodynamic Models: Review and New Perspectives

机译:NOS Galveston湾临近预报/预报系统的验证水动力模型:回顾和新观点

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The National Ocean Service (NOS) has developed an operationalnowcast/forecast system for Galveston Bay using a modified version of the Blumberg-Mellor (1987) three-dimensional hydrodynamic model extended to orthogonalcoordinates by Blumberg and Herring (1987) as discussed by Schmalz (1996, 2001). Thenowcast component works directly from the National Water Level Operational Networkdatabase using standardized readers. During the forecast component the NationalWeather Service's North American Mesoscale, River, and Extratropical Storm Surgemodels are used to provide the meteorological, surface water inflow, and Gulf of Mexicosubtidal water level forcings, respectively. In addition, a one-way coupled higherresolution Houston Ship Channel model (Schmalz, 2000) has also been incorporated intothe system. Hourly nowcasts of the previous 24 hour period and four times daily 30 hourforecasts of water surface elevation and currents, as well as three-dimensionaltemperature and salinity are performed using both bay and channel models.Initially, hindcast studies over June 1995, January 1995, October 1994, and April1996 were performed to validate the models for tidal and subtidal effects. Next, prior tooperational implementation, the experimental nowcast and forecast results were assessedover the one-year period April 2000 through March 2001 based on the NOS (1999)formal acceptance statistical criteria.The methods to estimate numerical uncertainty in computational fluid dynamiccomputations proposed by Roache (1997, 1998) are investigated as to theirappropriateness for these three-dimensional, unsteady, stratified, estuarine flow models.We first examine the basic procedures. Next we suggest how they might be applied to thebay and channel hydrodynamic model calculations. We consider both the hindcast andnowcast/forecast calculations. Potential difficulties and challenges are outlined for bothcalculation types. Finally, next steps are advanced to seek to improve the validationprocedure.
机译:国家海洋局(NOS)已发展了一项业务 加尔维斯顿湾的临近预报/预报系统,使用的是Blumberg- Mellor(1987)将三维流体动力学模型扩展到正交 由Schlumberz(1996,2001)讨论的Blumberg and Herring(1987)的坐标。这 临近预报组件直接从国家水位运营网络中工作 数据库使用标准化的读取器。在预报部分中,国家 气象局的北美中尺度,河流和温带风暴潮 模型用于提供气象,地表水流入量和墨西哥湾 潮下水位强迫。另外,单向耦合较高 分辨率休斯顿船舶航道模型(Schmalz,2000年)也已纳入 系统。前24小时时段的每小时临近预报,每天30小时,每天四次 预测水面高度和水流,以及三维 温度和盐度是使用海湾模型和河道模型进行的。 最初,在1995年6月,1995年1月,1994年10月和4月进行后验研究 1996年进行了潮汐和潮下影响模型的验证。接下来,之前 操作实施中,评估了实验性临近预报和预测结果 根据NOS(1999)在2000年4月至2001年3月的一年期间 正式的验收统计标准。 计算流体动力学数值不确定性的估算方法 研究了Roache(1997,1998)提出的计算方法 这些三维,不稳定,分层的河口水流模型的适用性。 我们首先检查基本程序。接下来,我们建议如何将它们应用于 海湾和河道水动力模型计算。我们既考虑了后遗症,也考虑了 临近预报/预测计算。概述了双方的潜在困难和挑战 计算类型。最后,推进下一步以寻求改进验证 程序。

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