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首页> 外文期刊>Journal of the Meteorological Society of Japan >Diagnosis of Large Prediction Errors on Recurvature of Typhoon Fengshen (2008) in the NCEP-GFS Model
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Diagnosis of Large Prediction Errors on Recurvature of Typhoon Fengshen (2008) in the NCEP-GFS Model

机译:NCEP-GFS模型中台风丰申(2008)重复预测误差的诊断

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The steering-flow analysis based on potential vorticity (PV) diagnosis is used to examine the reasons why the National Centers for Environmental Prediction Global Forecast System (NCEP-GFS) model showed large track forecast errors with over-recurving movement in Typhoon Fengshen (2008). In particular, two forecasts initialized at 0000 UTC 19 and 20 June 2008 are demonstrated in this study. The deep-layer-mean (DLM) steering flow between 925 and 300 hPa with tropical cyclone components filtered out is directed to the west or northwest in the analysis field, which can account for the continuous westward and northwestward movement in the best track. However, the DLM steering flow is shown more toward the north in the forecast fields. Four distinct PV features associated with the corresponding subtropical high, monsoon trough, continental high, and midlatitude trough are identified to diagnose their balanced steering flows around the storm. The result based on PV analysis indicates that the reduced westward steering flow in the forecast field is mainly attributed to the subtropical high which is over-predicted to extend southwestward, as well as the continental high with underestimated coverage, as characterized by the geopotential height at 500 hPa. The steering flow associated with the monsoon trough plays an essential role while Typhoon Fengshen (2008) experiences northward recurvature in both analysis and forecast fields. Therefore, the associated reduced westward steering flow in the NCEP-GFS model leads to the over-recurvature of Fengshen.
机译:基于潜在涡旋(PV)诊断的转向流量分析用于检查环境预测全球预测系统(NCEP-GFS)模型的国家中心的原因显示大轨预测误差,在台风丰申(2008年) )。特别是,在本研究中展示了在0000 UTC 19和2008年6月20日初始化的两种预测。在分析领域中滤过热带气旋组分的925和300hPa之间的深层平均值(DLM)转向流程,滤除了西部或西北部,可以考虑最佳轨道中的连续西向和西北运动。然而,DLM转向流程在预测领域的北方更像北方。鉴定了与相应的亚热带高,季风槽,大陆高和中光槽相关的四种不同的PV特征,以诊断风暴周围的平衡转向流。基于PV分析的结果表明,预测领域的减少的向西转向流量主要归因于亚热带高度,其过度预测扩展到西南部,以及低估的覆盖范围的大陆高度,如地质势高度所表征500 HPA。与季风槽相关的转向流量在台风凤山(2008)在分析和预测领域进行了向北重复性的同时发挥着重要作用。因此,NCEP-GFS模型中的相关减少的向西转向流导致丰申的过度重复。

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