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首页> 外文期刊>Quarterly Journal of the Royal Meteorological Society >Sensitivity experiments for ensemble forecasts of the extratropical transition of typhoon Tokage (2004)
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Sensitivity experiments for ensemble forecasts of the extratropical transition of typhoon Tokage (2004)

机译:台风Tokage温带过渡整体预报的敏感性实验(2004)

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The extratropical transition (ET) of tropical cyclones often has a detrimental impact on predictability in the vicinity of the event and downstream. Ensemble forecasts provide an appropriate means by which to investigate both the uncertainty and the dynamical development leading to the different ET scenarios. Sensitivity experiments are presented using the European Centre for Medium-Range Weather Forecasts (ECMWF) ensemble prediction system (EPS) to investigate different methods of perturbing the ensemble forecast of the ET of Typhoon Tokage (2004). During ET these perturbations have a notable impact on the ensemble spread representing the uncertainty. Three experiments were performed: one of them without singular vectors (SVs) targeted on the tropical cyclone, the second without stochastic physics and the third excluding both perturbation methods. The targeted perturbations are most important for sufficient spread in tfack and intensity. Without the targeted perturbations, the analysis is not contained within the ensemble spread. Stochastic physics leads to stronger reintensification of the ensemble members after ET. The higher track spread leads to higher variability in processes such as lower tropospheric latent heat release. This can be related to a higher spread in the upper-level midlatitude flow for both perturbation methods. A connection is drawn between the strength of ET and the modification of the downstream midlatitude flow pattern. The uncertainty due to the targeted perturbations propagates downstream with a Rossby wave train excited during Tokage's ET. For the case of stochastic physics, the uncertainty spreads to the ridge directly downstream of the ET system but is not evident further downstream.
机译:热带气旋的温带过渡(ET)通常会对事件附近和下游的可预测性产生不利影响。集合预报为调查导致不同ET情景的不确定性和动态发展提供了一种适当的手段。使用欧洲中距离天气预报中心(ECMWF)集合预报系统(EPS)进行了敏感性实验,以研究扰动台风(2004)ET集合预报的不同方法。在ET期间,这些扰动对表示不确定性的整体传播有显着影响。进行了三个实验:其中一个没有针对热带气旋的奇异矢量(SV),第二个没有随机物理学,第三个排除了两种扰动方法。有针对性的扰动对于tfack和强度的充分传播最重要。如果没有目标扰动,则分析不会包含在集合传播中。 ET之后,随机物理学导致集合成员的增强。较高的磁道扩展会导致过程中的可变性较高,例如对流层潜热释放较低。对于这两种扰动方法,这都可能与高层中纬度流的较高扩散有关。 ET的强度与下游中纬度流型的变化之间存在联系。在Tokage的ET期间,由目标扰动引起的不确定性在Rossby波列的作用下向下游传播。对于随机物理学的情况,不确定性直接在ET系统的下游扩散到山脊,但在下游则不明显。

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