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characteristics of evolution
相关语句
  演变特征
    DISTRIBUTION OF THE ATMOSPHERIC HEAT SOURCE AND ITS CHARACTERISTICS OF EVOLUTION OVER THE ASIAN MONSOON AREA BEFORE, IN AND AFTER MEIYU SEASON IN 1983
    1983年梅雨期前后亚洲季风区热源分布及其演变特征
短句来源
    Analysis on Characteristics of Evolution of Drought and Waterlogging Disasters in Henan
    河南旱涝灾害的演变特征分析
短句来源
    CLIMATOLOGICAL CHARACTERISTICS OF EVOLUTION OF EAST ASIAN WINTER MONSOON
    东亚冬季风的演变特征
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  characteristics of evolution
Furthermore, the characteristics of evolution for the disturbances of different modes in the hypersonic sharp cone boundary layer were discussed.
      
Changes in the quantitative characteristics of evolution of the phase variables (maximum Lyapunov exponent and Hausdorff dimension) are also studied as a function of the external field.
      


Characteristics of evolution of East Asia winter monsoon and cold surge were discussed and compared with those in South Asia. It is found that there exist an abrupt change of meridional circulation in East Asia during middle October, which represents the onset of East Asia winter monsoon circulation. Three abrupt changes of temperature occur in lower troposphere in the early September, middle November and late January. However, the change of the circulation in South Asia is not as strong as in East Asia....

Characteristics of evolution of East Asia winter monsoon and cold surge were discussed and compared with those in South Asia. It is found that there exist an abrupt change of meridional circulation in East Asia during middle October, which represents the onset of East Asia winter monsoon circulation. Three abrupt changes of temperature occur in lower troposphere in the early September, middle November and late January. However, the change of the circulation in South Asia is not as strong as in East Asia. The change of meridional wind in upper troposphere is earlier than that in lower troposphere. There exist two abrupt changes of the temperature in lower troposphere, which are weaker than in East Asia longitudinally. Furthermore, in East Asia, the frequency of cold surges has its maximum in South China Sea in December, but in west Pacific in January. On the other hand, in South Asia, the cold surges occur most frequently still in December , but much less than in East Asia, and they decrease quickly with time. Another different aspect is that the cold surge frequencies decrease upward in East Asia, but increase in South Asia.

文章主要讨论了东亚冬季风和冷涌的演变特征,并与南亚作了对比,发现在东亚地区,冬季风演变主要表现为10月中旬经向环流的突变及9月初、11月中旬和1月末对流层低层温度的3次突变;而在南亚地区,经向环流的变化不如东亚地区明显,而且高层要先于低层变化,对流层低层温度存在2次突变.在整个冬季,东亚地区冷涌的演变过程,主要表现为南海地区冷涌在12月份出现最高频率,而西太平洋冷涌在1月份出现最高频率;南亚地区冷涌在12月份出现最高频率,但远小于东亚地区且衰减速度很快.另一个不同点是东亚地区的冷涌强度是往上衰减的,而南亚地区的冷涌强度则是往上增强的.这说明东亚冬季风和南亚冬季风的性质有较大的区别

Heavy rain in southwest of South China caused by typhoon "Durian" is simulated by MM5. Based on the excellent agreement with the observation, the area average energetic budgets and conversion over the region of typhoon is undertaken with the balance equation of kinetic energy for the divergent wind and rotational wind, to indicate the maintaining mechanism of typhoon and the characteristic of evolution of energy, as well as the relationship between the typhoon and its outside enhanced heavy rain.

对 0 1 0 3号台风 (榴莲 )造成华南西南部特大暴雨的过程进行了高分辨数值模拟 ,在模拟结果与实况较为一致的基础上 ,利用辐散风和旋转风动能平衡方程分析低压区域内的动能收支和转换特征 ,揭示华南登陆台风低压衰减过程的能量演变特征及其与暴雨增幅关系

 
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