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首页> 外文期刊>Weather and forecasting >Forecasting Tropical Cyclones in the Western North Pacific Basin Using the NCEP Operational HWRF: Real-Time Implementation in 2012
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Forecasting Tropical Cyclones in the Western North Pacific Basin Using the NCEP Operational HWRF: Real-Time Implementation in 2012

机译:使用NCEP运行HWRF预测北太平洋西部盆地的热带气旋:2012年实时实施

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摘要

This study documents the recent efforts of the hurricane modeling team at the National Centers for Environmental Prediction's (NCEP) Environmental Modeling Center (EMC) in implementing the operational Hurricane Weather Research and Forecasting Model (HWRF) for real-time tropical cyclone (TC) forecast guidance in the western North Pacific basin (WPAC) from May to December 2012 in support of the operational forecasters at the Joint Typhoon Warning Center (JTWC). Evaluation of model performance for the WPAC in 2012 reveals that the model has promising skill with the 3-, 4-, and 5-day track errors being 125, 220, and 290 nautical miles (n mi; 1 n mi = 1.852 km), respectively. Intensity forecasts also show good performance, with the most significant intensity error reduction achieved during the first 24 h. Stratification of the track and intensity forecast errors based on storm initial intensity reveals that HWRF tends to underestimate storm intensity for weak storms and overestimate storm intensity for strong storms. Further analysis of the horizontal distribution of track and intensity forecast errors over the WPAC suggests that HWRF possesses a systematic negative intensity bias, slower movement, and a rightward bias in the lower latitudes. At higher latitudes near the East China Sea, HWRF shows a positive intensity bias and faster storm movement. This appears to be related to underestimation of the dominant large-scale system associated with the western Pacific subtropical high, which renders weaker steering flows in this basin.
机译:这项研究记录了美国国家环境预测中心(NCEP)环境建模中心(EMC)的飓风建模团队最近为实施实时热带气旋(TC)预报而实施的飓风天气研究和预报模型(HWRF)的努力2012年5月至12月在北太平洋西部盆地(WPAC)提供的指导,以支持联合台风预警中心(JTWC)的业务预报员。对2012年WPAC的模型性能进行评估后发现,该模型具有3天,4天和5天航迹误差为125、220和290海里(n mi; 1 n mi = 1.852 km)的技能很有希望, 分别。强度预测也显示出良好的性能,在最初的24小时内强度下降最大。基于风暴初始强度的航迹和强度预报误差的分层显示,对于弱风暴,HWRF倾向于低估风暴强度,而对于强风暴,HWRF倾向于高估风暴强度。在WPAC上对轨道和强度预报误差的水平分布的进一步分析表明,HWRF在较低的纬度上具有系统的负强度偏差,运动较慢和向右偏差。在东中国海附近的较高纬度处,HWRF显示出正的强度偏差和更快的风暴运动。这似乎与低估与西太平洋副热带高压有关的占主导地位的大型系统有关,这使该盆地的转向水流较弱。

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