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Statistical modelling of North Atlantic tropical cyclone tracks

机译:北大西洋热带气旋路径的统计模型

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We present a statistical model of North Atlantic tropical cyclone tracks from genesis site through lysis. To propagate tracks we use the means and variances of latitudinal and longitudinal displacements and model the remaining anomalies as autoregressive. Coefficients are determined by averaging near-neighbour historical track data, with 'near' determined optimally by using jackknife out-of-sample validation to maximize the likelihood of the observations. The number of cyclones in a simulated year is sampled randomly from the historical record, and the cyclone genesis sites are simulated with a spatial probability density function using kernels with optimized bandwidths. Simulated cyclones suffer lysis with a probability again determined from optimal averaging of historical lysis rates. We evaluate the track model by comparing an ensemble of 1950-2003 simulations to the historical record using several diagnostics, including landfall rates. In most regions, but not all, the observations fall within the variability across the ensemble members, indicating that the simulations and observations are statistically indistinguishable. An intensity component to the TC model, necessary for risk assessment applications, is currently under development.
机译:我们提出了一个北大西洋热带气旋径迹的统计模型,其起源是通过裂解。为了传播轨迹,我们使用纬向和纵向位移的均值和方差,并将剩余异常建模为自回归模型。系数是通过平均近邻历史轨道数据来确定的,“近”值是通过使用折刀的样本外验证来最大程度地确定观测结果的。从历史记录中随机抽取模拟年份的气旋数量,并使用具有优化带宽的内核以空间概率密度函数模拟气旋的发生地点。模拟旋风分离器遭受裂解的可能性再次由历史裂解速率的最佳平均值确定。我们通过比较1950-2003年模拟的集合与历史记录(使用多种诊断方法,包括降落率)来评估轨道模型。在大多数区域(但不是全部)中,观测值落在整个集合成员的变异性之内,这表明模拟和观测值在统计上是无法区分的。目前正在开发风险评估应用所需的TC模型强度组件。

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