首页> 外文期刊>Journal of Hydrology >Error characterization of ARW model in Forecasting tropical cyclone rainfall over North Indian Ocean
【24h】

Error characterization of ARW model in Forecasting tropical cyclone rainfall over North Indian Ocean

机译:ARW模式在北印度洋热带气旋降雨预报中的误差表征

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

The hydrological extremes due to the landfalling tropical cyclones (TCs) pose a severe threat to the coastal communities over the North Indian Ocean (NIO) region. Advanced Research Weather Research and Forecasting (ARW) model is obscure in rainfall prediction, while it is extensively evaluated for track and intensity prediction over the NIO. This study focuses on estimating the model rainfall errors based on a total of 280 TC forecast cases from 42 TCs from 2007 to 2018. The model rainfall errors are studied against rain gauge and Tropical Rainfall Measuring Mission (TRMM) data as a function of TC intensity stage and model forecast length. The short-range (24 h) rainfall guidance yields fewer errors than the long-range (48-96 h) forecast when the model is initialized at any TC intensity stage. The root mean square error (RMSE) and bias of ARW rainfall is higher when the model is initialized at weaker intensity (DD or CS) stages than initialized at stronger intensity (SCS and VSCS) stages. The inland rainfall errors increase with forecast lead. The model exhibited higher errors (~2 mm h~(-1)) in the inner-core region (0-100 km) and lesser errors (~0.5 mm h~(-1)) in the TC environment (200-400 km). The ARW model replicates the observed radial profiles of rainfall up to 400 km with 2-5 mm h~(-1) overestimation at different intensity stages. Rainfall error decomposition of contiguous rain area (CRA) analysis indicates that the pattern errors contribute the maximum (~50) to the total error, followed by the displacement error (~35). In comparison, the volume and rotational errors are less (10 and 2, respectively). The mean CRA horizontal shift in rainfall decreases from weaker to stronger stage initialization. The radial-distance error of categorical rainfall distribution between the ARW model and TRMM is ~ 150-200 km. This error reduced to 20-50 km after correcting the model rainfall for CRA displacement errors. The RMSE of model-rainfall after CRA correction has red
机译:热带气旋(TCs)登陆导致的极端水文对北印度洋(NIO)地区的沿海社区构成严重威胁。Advanced Research Weather Research and Forecasting (ARW) 模型在降雨预报方面存在模糊性,而在 NIO 的路径和强度预测方面却对其进行了广泛的评估。本研究基于2007—2018年42个TC的280个TC预报案例,估算模型降雨误差。根据雨量计和热带降雨测量任务(TRMM)数据,研究了模型降雨误差,作为TC强度阶段和模型预报长度的函数。当模型在任何 TC 强度阶段初始化时,短期 (24 h) 降雨指导产生的误差比长期 (48-96 h) 预测的误差要小。当模型在弱强度(DD或CS)阶段初始化时,ARW降雨的均方根误差(RMSE)和偏差高于在强强度(SCS和VSCS)阶段初始化的模型。内陆降雨误差随预报超前而增加。该模型在内核区(0-100 km)的误差较高(~2 mm h~(-1)),在TC环境(200-400 km)的误差较小(~0.5 mm h~(-1))。ARW模型复制了观测到的400 km以2-5 mm h~(-1)高估了不同强度阶段降雨的径向剖面。连续降雨区(CRA)分析的降雨误差分解表明,模式误差对总误差的贡献最大(~50%),其次是位移误差(~35%)。相比之下,体积误差和旋转误差较小(分别为 10% 和 2%)。平均CRA水平降水量水平移动由弱到强逐渐减少。ARW模式与TRMM分类降雨分布的径向距离误差为~150-200 km。在校正了CRA位移误差的模型降雨量后,该误差减少到20-50 km。CRA校正后模式降雨量RMSE为红色

著录项

获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号