Tropical cyclone forecasts for the Western North Pacific with high-resolution atmosphere and coupled atmosphere-ocean models

Q4 Earth and Planetary Sciences Papers in Meteorology and Geophysics Pub Date : 2018-01-01 DOI:10.2467/MRIPAPERS.67.15
Kosuke Ito, M. Sawada, M. Yamaguchi
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Abstract

This work quantified the skills of high-resolution regional nonhydrostatic models in forecasting tropical cyclones (TCs) in the Western North Pacific. The selected cases were almost all TCs during 2012–2014 with an initial time of 1200 UTC. The Japan Meteorological Agency (JMA)-nonhydrostatic model with a horizontal grid spacing of 5 km (NHM5km_atm) and its atmosphere-ocean coupled version (NHM5km_cpl) were used to conduct three-day forecasts. The JMA-global spectral model (GSM) outputs interpolated to a horizontal grid spacing of 0.5 degree were used for initial and lateral boundary conditions of the NHM5km_atm and NHM5km_cpl. The skills and GSM forecast skill were validated with respect to the Regional Specialized Meteorological Center Tokyo best track dataset. Results showed that use of the NHM5km_atm and NHM5km_cpl generally improved track forecasts at forecast times of 24–60 h. Track forecasts improved by as much as 20% for TCs with strong vertical shears of horizontal winds. However, a two-tailed test for the mean value revealed that the improvements were not statistically significant above the 90% confidence level. Use of the NHM5km_atm and NHM5km_cpl significantly improved TC intensity forecasts of 2–3 days by more than 20% with respect to the GSM, but strong TC intensities were not well predicted by short-term forecasts because of initialization deficiencies. Although the NHM5km_cpl tended to seriously underestimate TC intensities, it tended to produce the greatest increase in the correlation coefficient between observed and predicted intensity changes. This study also showed that the method used to determine the TC center position affects the track forecast error by up to a few percent and that the maximum wind speed forecast error depends on the best track dataset selected as a reference.
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用高分辨率大气和大气-海洋耦合模式预报西北太平洋热带气旋
这项工作量化了高分辨率区域非流体静力模式在预测北太平洋西部热带气旋(tc)方面的技能。所选病例几乎全部为2012-2014年期间的tc,初始时间为UTC时间1200。利用日本气象厅(JMA)水平网格间距为5km的非流体静力模式(NHM5km_atm)及其大气-海洋耦合模式(NHM5km_cpl)进行了为期3天的预报。利用插值到0.5度水平网格间距的JMA-global spectral model (GSM)输出对NHM5km_atm和NHM5km_cpl的初始边界条件和侧向边界条件进行了研究。在区域专业气象中心东京最佳航迹数据集上验证了该技能和GSM预报技能。结果表明,NHM5km_atm和NHM5km_cpl在24 ~ 60 h的预报时间内总体上改善了路径预报,对于水平风强垂直切变的tc,路径预报提高了20%。然而,对平均值的双尾检验显示,在90%的置信水平之上,改善在统计学上并不显著。NHM5km_atm和NHM5km_cpl对2 ~ 3 d TC强度的预报较GSM提高了20%以上,但由于初始化不足,短期预报对强TC强度的预报效果较差。NHM5km_cpl虽然严重低估了TC强度,但其对TC强度变化的相关系数增加幅度最大。研究还表明,确定TC中心位置的方法对路径预报误差的影响可达几个百分点,最大风速预报误差取决于所选择的最佳路径数据集作为参考。
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来源期刊
Papers in Meteorology and Geophysics
Papers in Meteorology and Geophysics Earth and Planetary Sciences-Geophysics
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