Ni Yunqi, Zhou Xiuji. 2004: STUDY FOR FORMATION MECHANISM OF HEAVY RAINFALL WITHIN THE MEIYU FRONT ALONG THE MIDDLE AND DOWNSTREAM OF YANGTZE RIVER AND THEORIES AND METHODS OF THEIR DETECTION AND PREDICTION. Acta Meteorologica Sinica, (5): 647-662. DOI: 10.11676/qxxb2004.063
Citation: Ni Yunqi, Zhou Xiuji. 2004: STUDY FOR FORMATION MECHANISM OF HEAVY RAINFALL WITHIN THE MEIYU FRONT ALONG THE MIDDLE AND DOWNSTREAM OF YANGTZE RIVER AND THEORIES AND METHODS OF THEIR DETECTION AND PREDICTION. Acta Meteorologica Sinica, (5): 647-662. DOI: 10.11676/qxxb2004.063

STUDY FOR FORMATION MECHANISM OF HEAVY RAINFALL WITHIN THE MEIYU FRONT ALONG THE MIDDLE AND DOWNSTREAM OF YANGTZE RIVER AND THEORIES AND METHODS OF THEIR DETECTION AND PREDICTION

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  • Received Date: August 26, 2004
  • Revised Date: September 12, 2004
  • Published Date: February 19, 2013
  • The project on study for formation mechanism and theories and methods of detection and prediction of severe weather disasters in China from National Key Basic Research Development Program has been studied by all the scientists of this project for five years. It has been made important progresses including six aspects related to heavy rainfall: (1) Muti-scales physical models of heavy rainf all within the Meiyu front based on the real-time observed data have been proposed; (2) It has established a synoptic model for heavy rainfall within the Meiyu front; (3) Meiyu front is Meiyu frontal system which consists of multi-synoptic systems with different spacetime scales. It has structure characteristics of subtropical frontal system which is between structure characteristics of extra-tropical frontal system and ITCZ. However, sometime it has dual-peaks structure in the middle-downstream of Yangtze River. And its mainenance and development mechanism has also been discussed. (4) Several kinds of quantitative remote sensing retrieval theories and methods have been proposed for meso-scale heavy rainfall; (5) Dual-Dopplor detecting methods and retrieval theories for meso scale heavy rainfall have successfully been studied. (6) The meso scale heavy rainfall numerical prediction model system with 3Dvar has been developed. The above progresses showed that the project on heavy rainfall study has been reached to the goals and finished the tasks in the last five years. It is substantial scientific base for advancing deeply studying of heavy rainfall in China.
  • 赵思雄,陶祖钰,孙建华等.长江流域梅雨锋暴雨机理的分析研究.见:倪允琪,周秀骥主编.国家重点基础研究发展规划项目<我国重大天气灾害形成机理与预测理论研究>研究专著系列丛书之一.北京:气象出版社,2004.282pp
    陶诗言,张小玲,张顺利.长江流域梅雨锋暴雨灾害研究.见:倪允琪,周秀骥主编.国家重点基础研究发展规划项目<我国重大天气灾害形成机理与预测理论研究>研究专著系列丛书之二.北京:气象出版社,2004.192pp
    陶诗言,倪允琪,赵思雄等.1998夏季中国暴雨形成机理与预报研究.北京:气象出版社,2001.1~184
    Jiang Jianyin,Ni Yunqi.Diagnostic study on the structure characteristics of a typical Mei-Yu Front System and Its Maintenance Mechanism.Adv Atmos Sci,2004,21(5):1~12
    伍荣生,高守亭,谈哲敏等.锋面过程与中尺度扰动.见:倪允琪,周秀骥主编.国家重点基础研究发展规划项目<我国重大天气灾害形成机理与预测理论研究>研究专著系列丛书之三.北京:气象出版社,2004.170pp
    张文建,许健民,方宗义等.暴雨系统的卫星遥感理论和方法.见:倪允琪,周秀骥主编.国家重点基础研究发展规划项目<我国重大天气灾害形成机理与预测理论研究>研究专著系列丛书之四.北京:气象出版社,2004.427pp
    Xu J,Holmlund K,Zhang Q,et al.Comparison of two schemes for derivation of atmospheric motion vectors.Geophys Rese,2002,107 (14D):ACL 4-1~4-15
    程明虎,刘黎平,张沛源等.暴雨系统的多普勒雷达反演理论和方法.见:倪允琪,周秀骥主编.国家重点基础研究发展规划项目<我国重大天气灾害形成机理与预测理论研究>研究专著系列丛书之五.北京:气象出版社,2004.252pp
    宇如聪,薛纪善,徐幼平等.AREMS中尺度暴雨数值预报模式系统.见:倪允琪,周秀骥主编.国家重点基础研究发展规划项目<我国重大天气灾害形成机理与预测理论研究>研究专著系列丛书之六.北京:气象出版社,2004.232pp
    倪允琪,刘黎平,高梅等.长江中下游梅雨锋暴雨野外科学试验.见:倪允琪,周秀骥主编.国家重点基础研究发展规划项目<我国重大天气灾害形成机理与预测理论研究>研究专著系列丛书之八.北京:气象出版社,2004.208pp.

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