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Development of a coupled atmosphere-ocean typhoon regional assimilation and prediction system for operational typhoon forecasting by the Chinese Academy of Meteorological Sciences-part Ⅰ: experiments of Western North Pacific typhoons in 2016

机译:中国气象科学院耦合大气 - 海风区域同化和运营台风预测预测系统的研制 - 第Ⅰ:2016年西北太平洋台风的实验

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摘要

Typhoons can interact intensely with oceans, and the atmosphere-ocean interaction has an enormous impact on the intensity and structure of typhoons. To consider the impact of typhoon-ocean interactions, a regional coupled atmosphere-ocean system for operational forecasting of Western North Pacific typhoons is established in this paper based on a public coupled atmosphere-ocean framework and in accordance with the operational typhoon forecasting conditions and system settings of the Chinese Academy of Meteorological Sciences. The new coupled system is fully validated and used for hindcasting experiments on all typhoons in 2016. The results show that the computational cost associated with the proposed coupled system is approximately 5.33 times that of the atmosphere-only system. A comparison of the hindcasts of the 2016 typhoons using the atmosphere-only system and the proposed coupled system reveals that the use of the coupled system can obviously reduce the forecasted intensity error by approximately 10-20% but not the typhoon track error. In addition, some of the intrinsic structural characteristics of typhoons influence the effectivity of the coupled system. Specifically, when typhoons have a high intensity and a low transla-tional speed, move in an East-West or turning direction, and are at 20°N-25°N latitude, the forecasts can be relatively significantly improved by the coupled system; otherwise, the improvement is not obvious.
机译:台风可以与海洋强烈相互作用,大气 - 海洋互动对台风的强度和结构产生了巨大影响。要考虑台风 - 海洋互动的影响,基于公共耦合的大气框架,并根据运营台风预测条件和制度,在本文建立了一个区域北太平洋台风运营预测的区域耦合大气 - 海洋系统。中国气象科学院的环境。新耦合系统完全验证并用于2016年所有台风的后传播实验。结果表明,与所提出的耦合系统相关的计算成本约为大气系统的5.33倍。通过仅使用大气系统和所提出的耦合系统的2016台台风的Hindcasts的比较揭示了耦合系统的使用明显将预测的强度误差减少约10-20%但不是台风轨迹误差。此外,台风的一些内在结构特征影响了耦合系统的有效性。具体地,当台风具有高强度和低透气速度时,在东部或转向方向上移动,并且在20°N-25°N纬度下,通过耦合系统可以相对显着地改善预测;否则,改善并不明显。

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