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hurricane waves
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  “hurricane waves”译为未确定词的双语例句
     THE CHARACTERISTICS OF HURRICANE WAVES IN NANJI SEA AREA
     南麂海域台风影响过程中的波浪特征
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  相似匹配句对
     VORTEX ROSSBY WAVES IN HURRICANE
     飓风中的涡旋罗斯贝波
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     Hurricane
     飓风
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     THE CHARACTERISTICS OF HURRICANE WAVES IN NANJI SEA AREA
     南麂海域台风影响过程中的波浪特征
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     Radio Waves
     无线电波
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     POWER WAVES
     (威力波)横空问世
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  hurricane waves
Conversely the effects of hurricane waves in 1982 and 1992 together caused major physical destruction to the reefs.
      


This paper presents a series of formulas to statistically predict design extreme values for four different situations; ( a ) short-term prediction; ( b ) long-term prediction from daily maximum wave heights, which has initial distribution as log-normal distribution) ( c ) long-term prediction from typhoon (or hurricane) wave heights, initial distribution of which has Gumbel (or Weibull) distribution) ( d ) long-term prediction from annual maximum wave heights. Difference between these...

This paper presents a series of formulas to statistically predict design extreme values for four different situations; ( a ) short-term prediction; ( b ) long-term prediction from daily maximum wave heights, which has initial distribution as log-normal distribution) ( c ) long-term prediction from typhoon (or hurricane) wave heights, initial distribution of which has Gumbel (or Weibull) distribution) ( d ) long-term prediction from annual maximum wave heights. Difference between these new formulas and formulas used in ocean engineering is that calculated results by past formulas are probable extreme value, which has risk probability 0.632, but new type of formulas includes design return period and risk probability, therefore they can be used for predict design extreme value for different return period and risk probability.

本文提出一组在四种不同情况下之波浪长期极值计算公式。由于公式中既包含了设计要求之重现期,又体现了可能遭受破坏的危险率,故可用于海洋动力现象的设计极值推算。

According to observational data during 1960-1989 at Naji Oceanographic Station, the characteristics of wind and wave in the area are analysed. The results show the wave in the area is usually mixing type with wave height often being force-three. The mean distribution of wave elements is smooth while the distribution extremes uneven. The union distribution indicates that the frequency peak of occurrence falls on the kind of wave of 0. 5~1. 9m in height, 4. 0 - 6. 9s in period. The...

According to observational data during 1960-1989 at Naji Oceanographic Station, the characteristics of wind and wave in the area are analysed. The results show the wave in the area is usually mixing type with wave height often being force-three. The mean distribution of wave elements is smooth while the distribution extremes uneven. The union distribution indicates that the frequency peak of occurrence falls on the kind of wave of 0. 5~1. 9m in height, 4. 0 - 6. 9s in period. The basic change cycle about wave height, period and wind speed is obtained using the method of largest entropy spectral analysis. The empirical relationship between period and largest wave height of the hurricane wave is discussed.

根据1960~1989年南麂海洋站的实测风浪资料,分析了该海域的风浪特征,结果认为:这个海域的浪通常是混合浪,常见浪是三级波高的浪;海浪要素的均值分布比较平稳,极值具有不均匀分布的特性.本区的波高和周期的联合分布表明,波高在0.5~1.9m,周期为4.0~6.9s类型的浪在该海域出现频率最高.此外,引用最大熵谱方法找出了本区波高、周期和风速的主要变化周期.还讨论了台风浪的周期与最大波高的经验关系.

Based on observational data of hurricane wave at Nanji oceanographic station between 1983-1989, the evolvements of observational wave pattern in hurricane wave are analysed. The relationships between wave slope and wave pattern and that between wind speed and wave pattern are discussed. The results show that wave pattern of larger wave in the region is largely that of wind wave and , when wind speed over Beaufort force six, totally that of wind wave....

Based on observational data of hurricane wave at Nanji oceanographic station between 1983-1989, the evolvements of observational wave pattern in hurricane wave are analysed. The relationships between wave slope and wave pattern and that between wind speed and wave pattern are discussed. The results show that wave pattern of larger wave in the region is largely that of wind wave and , when wind speed over Beaufort force six, totally that of wind wave. It can be concluded that the hurricane wave of different reappearance is wind wave.

以南麂海洋站1983~1989年实测台风波浪资料为依据,分析了台风影响过程中测点波型的演变,对台风浪的波陡与波型、风速与波型之间的关系进行讨论.从而得出,台风影响过程中本区出现较大波浪的波型绝大部分属于风浪,6级以上风速作用时,本区台风浪均属于风浪波型,从而可以断定,不同重现期的台风波浪应属于风浪.

 
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