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An Application of the Adjoint Method to a Statistical-Dynamical Tropical-Cyclone Prediction Model (SD-90) Ⅱ: Real Tropical Cyclone Cases
引用本文:项杰,廖前锋,黄思训,兰伟仁,冯强,周凤才.An Application of the Adjoint Method to a Statistical-Dynamical Tropical-Cyclone Prediction Model (SD-90) Ⅱ: Real Tropical Cyclone Cases[J].大气科学进展,2006,23(1):118-126.
作者姓名:项杰  廖前锋  黄思训  兰伟仁  冯强  周凤才
作者单位:[1]Institute of Meteorology, PLA University of Science and Engineering, Nanjing 211101 [2]Shanghai Institute of Typhoons, Shanghai 200030 [3]Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 [4]Shanghai Meteorological Center, Air Traffic Management Bereau of East China, Shanghai 200066
基金项目:Acknowledgments. Sincere appreciation is due to the two anonymous referees for their valuable suggestions. This work was supported jointly by the Typhoon Foundation of Shanghai, by LASC of the Institute of Atmospheric Physics of the Chinese Academy of Sciences, and by the National Natural Science Foundation of China under Grant No. 40633030.
摘    要:In the first paper in this series, a variational data assimilation of ideal tropical cyclone (TC) tracks was performed for the statistical-dynamical prediction model SD-90 by the adjoint method, and a prediction of TC tracks was made with good accuracy for tracks containing no sharp turns. In the present paper, the cases of real TC tracks are studied. Due to the complexity of TC motion, attention is paid to the diagnostic research of TC motion. First, five TC tracks are studied. Using the data of each entire TC track, by the adjoint method, five TC tracks are fitted well, and the forces acting on the TCs are retrieved. For a given TC, the distribution of the resultant of the retrieved force and Coriolis force well matches the corresponding TC track, i.e., when a TC turns, the resultant of the retrieved force and Coriolis force acts as a centripetal force, which means that the TC indeed moves like a particle; in particular, for TC 9911, the clockwise looping motion is also fitted well. And the distribution of the resultant appears to be periodic in some cases. Then, the present method is carried out for a portion of the track data for TC 9804, which indicates that when the amount of data for a TC track is sufficient, the algorithm is stable. And finally, the same algorithm is implemented for TCs with a double-eyewall structure, namely Bilis (2000) and Winnie (1997), and the results prove the applicability of the algorithm to TCs with complicated mesoscale structures if the TC track data are obtained every three hours.

关 键 词:热带气旋  伴随矩阵  预测模型  TC模型
收稿时间:2005-02-25
修稿时间:2005-11-16
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