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Simulations of the 26 December 2004 Indian Ocean tsunami using amulti-purpose Ocean disaster simulation and prediction model

机译:使用多用途海洋灾害模拟和预测模型模拟2004年12月26日印度洋海啸

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Under Advanced Ocean State Forecast activity at MOG/SAC, a comprehensive multi-model ensemble called TOAST comprising an ocean general circulation model, a coastal surge and tide prediction model coupled with a suitable cyclone prediction model is being tested. The model is designed specifically to simulate and predict ocean disasters like storm surge, etc. The model has flexible grids structure and apart from calculation of the surge height, it also provides the area of intense inundation in the coastal region. The ocean general circulation component of TOAST has a very clear separation of the barotropic and baroclinic modes of energy propagation. Due to this separation, it is possible to configure the model to retain very fast gravity waves, which are generally filtered away in studies connected with OGCM, and hence indicating a possibility to simulate tsunami. The 26 December 2004 Indian Ocean tsunami has been used as the case study to see the whole life cycle from generation to runaway using this model. The earthquake data has been converted into the model-required parameters using an elastic plate movement model employed for most of the earthquake studies. We have assumed the quake intensity at Richter scale 9.0 occurring at 0056 UTC and compared the simulation with Jason altimeter pass in the central Bay of Bengal at 0256 UTC. The results are very encouraging. The model simulations, even with the complication of a normal general circulation model, take about 180 min CPU time on a 4-CPU Itenium-2 machine at 9 km resolution, and therefore, has the potential of an operational mode system using faster computer systems.
机译:在MOG / SAC进行的高级海洋状态预报活动下,正在测试一个称为TOAST的综合多模型集合,该集合包括海洋一般环流模型,沿海潮汐和潮汐预测模型以及合适的气旋预测模型。该模型是专门为模拟和预测风暴潮等海洋灾害而设计的。该模型具有灵活的网格结构,除计算浪涌高度外,还提供了沿海地区被大量淹没的区域。 TOAST的海洋总环流成分将正,负斜向能量传播模式非常清楚地分开了。由于这种分离,可以将模型配置为保留非常快的重力波,重力波通常在与OGCM相关的研究中被滤除,因此表明有可能模拟海啸。使用2004年12月26日的印度洋海啸作为案例研究,使用该模型可以看到从一代到失控的整个生命周期。使用大多数地震研究中使用的弹性板运动模型,已将地震数据转换为模型所需的参数。我们假设发生在0056 UTC的里氏9.0级地震强度,并且将该模拟与0256 UTC的孟加拉中央海湾的Jason高度计通过进行了比较。结果非常令人鼓舞。即使使用普通的通用循环模型,模型仿真也需要花费9分钟的分辨率在4-CPU Itenium-2机器上花费约180分钟的CPU时间,因此具有使用较快计算机系统的操作模式系统的潜力。

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