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DYNAMIC CALCULATION RANGE TYPE NUMERICAL SIMULATION METHOD OF TSUNAMI BASED ON FLUX

机译:基于通量的海啸动态计算范围数值模拟方法

摘要

PURPOSE: A flow rate base working area variable form seismic surges value holding method is provided to drastically shorten value imitation turnaround time of the seismic surges. CONSTITUTION: A flow rate base working area variable form seismic surges value holding method comprises the following steps: setting initial physical quantity for each grid point which includes depth of water; calculating difference formula and producing the boating amount and depth of water; unconditionally repeating the calculation if the calculation object grid point position is less than the flooding determination load point; conditionally repeating the calculation if calculated object grid point position is greater than the flooding determination load point; changing the flooding determination load point into the current calculation object grid point position if the calculated object grid point position is higher than the flooding determination load point and the calculated depth of water is 0 or less; changing the flooding determination load point into the position which antidromically moves the street corresponding to the double of the boating amount and scale factor from the current calculation object grid point position if the boating amount of the just before grid point is 0 or less; and calculating the renewed calculation time after restoring back the calculation object grid point to the origin. [Reference numerals] (AA) Start; (BB) End; (CC) Calculation grid point = flooding determination load point; (DD) Depth of water of the calculation grid point 0; (EE) Linear flow rate of the calculation grid point = 0; (FF) Calculation time = end time; (S10) Setting initial flooding determination load points, scale factors, and initial values for each grid point; (S20) Operating a difference formula and calculating the line flow rate and the depth of water of the calculation grid point; (S31,S32) Moving the calculation grid point to the forward direction; (S41) Flooding determination load point = current calculation grid point; (S42) Flooding determination load point = current calculation grid point + scale factor x the linear flow rate of the calculation grid point; (S50) Updating the calculation time and returning the calculation grid point to the origin
机译:目的:提供一种流量基础工作区域可变形式的地震波数值保持方法,以大大缩短地震波的数值模拟周转时间。构成:流量基础工作区可变形式的地震浪涌值保持方法包括以下步骤:为每个网格点设置包括水深的初始物理量;计算差公式并产生划船量和水深;如果计算对象网格点位置小于淹没判定负荷点,则无条件重复计算。如果计算出的目标网格点位置大于淹没确定载荷点,则有条件地重复计算;如果计算出的目标网格点位置高于淹没确定负荷点并且计算出的水深为0以下,则将淹没确定载荷点改变为当前计算目标网格点位置;如果紧邻前网格点的划船量为0以下,则将淹没确定负荷点改变为从当前计算对象网格点位置使与划船量和比例因子的倍数相对应的街道逆行移动的位置;将计算对象网格点恢复到原点后,计算更新后的计算时间。 [参考数字](AA)开始; (BB)结束; (CC)计算网格点> =洪水确定荷载点; (DD)计算格网点的水深> 0; (EE)计算网格点的线性流速<= 0; (FF)计算时间=结束时间; (S10)为每个网格点设置初始洪水确定载荷点,比例因子和初始值; (S20)运算差分公式,计算出计算格点的线流量和水深; (S31,S32)将计算网格点向前移动; (S41)淹没判定负荷点=当前计算网格点; (S42)注水判定负荷点=当前计算网格点+比例因子×计算网格点的线性流量。 (S50)更新计算时间并将计算网格点返回原点

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