北印度洋热带气旋强度预测——基于NWP的客观方法

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geofizika Pub Date : 2019-01-14 DOI:10.15233/GFZ.2018.35.8
S. Bhattacharya, S. D. Kotal, S. Nath, S. Bhowmik, P. K. Kundu
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引用次数: 0

摘要

本文探讨了一种基于数值天气预报(NWP)的客观强度预测方法,利用ECMWF模式输出对北印度洋(NIO)热带气旋强度进行预测。根据世界气象组织(WMO),热带气旋的强度是以最大持续风力(平均10分钟)来划分的。利用2010-2012年期间的100多次分析,建立了系统中心周围6°× 6°格框内模式最大平均海平面压力(MSLP)与系统中心最低平均海平面压力(ΔP)的差值与观测强度之间的经验关系。同样的方法也用于预测2014年在孟加拉湾观测到的非常严重的气旋风暴Hudhud和深度低气压的强度。结果表明,与使用不同K常数值的Vmax = K DP关系进行预测相比,经验方程能够较好地预测强度。误差分析表明,使用本文导出的经验方程进行强度预测的相对误差比使用K = 14.2 kt / hPa进行强度预测的相对误差小34%,在0.95水平上有显著改善。
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Tropical cyclone intensity prediction over the North Indian Ocean - An NWP based objective approach
A Numerical Weather Prediction (NWP) based objective intensity prediction approach has been explored for prediction of tropical cyclone intensity over the North Indian Ocean (NIO) using ECMWF model outputs. The intensity of a tropical cyclone is classified by the maximum sustained wind (10-min mean) according to World Meteorological Organization (WMO). An empirical relationship between the difference of the model’s maximum mean sea level pressure (MSLP) inside a 6° × 6° grid box around the centre of the system and the lowest mean sea level pressure at the centre of the system (ΔP) with the observed intensity is developed using over 100 analyses during 2010–2012. The same is used to predict intensity of very severe cyclonic storm Hudhud and a Deep Depression observed over the Bay of Bengal during 2014. The results show that the empirical equation is skillful in prediction of intensity as compared to predictions computed using the relationship Vmax = K DP with different constant values of K. The error analyses show that the relative error in intensity prediction using the empirical equation derived in the present study is 34% less than the same using K = 14.2 kt / hPa in Vmax = K DP with an improvement which is significant at the level of 0.95.
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来源期刊
Geofizika
Geofizika 地学-地球化学与地球物理
CiteScore
1.60
自引率
0.00%
发文量
17
审稿时长
>12 weeks
期刊介绍: The Geofizika journal succeeds the Papers series (Radovi), which has been published since 1923 at the Geophysical Institute in Zagreb (current the Department of Geophysics, Faculty of Science, University of Zagreb). Geofizika publishes contributions dealing with physics of the atmosphere, the sea and the Earth''s interior.
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