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Research into Wave Energy Characteristic Signal of Transition Rainfall in Summer Drought Period in Sichuan and Chongqing

机译:四川和重庆夏季干旱期过渡降雨波能特性信号研究

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Based on NCEP/NCAR reanalysis materials and wave-packet propagation diagnosis (WPD) method, this paper focuses on research into wave energy distribution and propagation features during two transition rainfall process in summer drought period in Sichuan and Chongqing in 2006. The result shows that two transition rainfall processes witnessed basically consistent wave energy evolution in middle and low layer. Before rainfall, wave-packet developed a lot in Arabian Sea region and strong wave-packet center was propagated to south of the plateau and moved to west of Sichuan and the wave-packet center of West Pacific was propagated northwest. At the time of rainfall, wave-packet was slightly reduced in Arabian Sea region but was still in strong phase in south of the plateau region. East and middle of Sichuan and Chongqing suffering rainfall was large wave-packet value areas due to impact of wave-packet propagation from West Pacific. During the rainfall, the wave-packet was propagated from Arabian Sea and West Pacific to south of the plateau and east and middle of Sichuan and Chongqing respectively. East and middle of Sichuan and Chongqing are under control of large wave-packet value areas, with heavy rain. At the ending of rainfall, wave-packet in Arabian Sea and West Pacific was gradually reduced and wave-packet propagation in south of the plateau, Sichuan and Chongqing was weakened. At ending of rainfall, wave-packet in Sichuan and Chongqing was weakened into small value. According to analysis, during the first rainfall, the wave-packet value in middle layer was stronger than that in low layer in Sichuan and Chongqing. During the second rainfall, wave-packet was stronger than that in the first rainfall process in general, the wave-packet in low layer was slightly stronger than that in middle layer, but the second rainfall was far heavier than the first rainfall. In general, wave-packet strength and propagation is related with two transition rainfalls in summer drought pe- - riod in 2006. Obvious characteristic signal was shown in terms of its generation, lasting, ending and strength, which shows that wave energy signal is meaningful for prediction.
机译:基于NCEP / NCAR再分析材料和波浪分组传播诊断(WPD)方法,本文重点介绍了在2006年夏季及重庆夏季干旱期间两次过渡降雨过程中的波能量分布和传播特征的研究。结果表明两种过渡降雨过程目睹了中低层基本一致的波能量演化。在降雨之前,波浪包在阿拉伯海地区开发了很多,强大的波浪包中心被宣传到高原南部,搬到四川以西,西太平洋的波浪包中心繁殖西北部。在降雨时,阿拉伯海地区的波浪包略微减少,但在高原地区的南部仍然处于强劲的阶段。四川东部和中部,重庆遭受降雨量是大波浪包价值领域,由于West Pacific的波浪包传播的影响。降雨期间,波浪包分别从阿拉伯海和西太平洋到四川和重庆的东部和中部。四川和重庆的东部和中部都在控制大波浪包价值区域,大雨。在降雨结束时,阿拉伯海和西太平洋的波浪包在高原南部的逐渐减少,四川和重庆的南部繁殖。在降雨结束时,四川和重庆的波浪包被削弱成小价值。根据分析,在第一次降雨期间,中间层中的波浪分组值比四川和重庆的低层强。在第二次降雨期间,波浪包比第一降雨过程中的较强,一般而言,低层的波浪包略强于中间层,但第二次降雨量比第一次降雨量重得多。一般来说,波浪分组强度和传播与2006年夏季干旱PE-Riod中的两种过渡降雨有关。以其一代,持久,结束和强度而言,显示了明显的特征信号,表明波能量信号有意义预测。

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