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1)  predication equation for significant wave height
台风浪波高估算
2)  typhoon wave
台风波浪
1.
Typhoon waves (including tropical storm waves and severe tropical storm waves) at certain observation points in shantou coastal areas have been selected by the authors to study the following 3 aspects: (1)analysis of in situ observed records; (2)hindcasting of typhoon waves and their basic characteristics; and (3) determining each typhoon wave element in various recurrence periods.
作者选择了汕头近岸区某测点的台风(包括热带风暴和强热带风暴,下同)波浪从下列三个方面进行分析研究:(一)实测记录的分析;(二)后报台风波浪及其基本特征;(三)各种重现期台风波浪要素的确定。
2.
The paper analyzes the typhoon waves of survey site W1 at the mouth of theDaya Bay and W2 inside the bay, and compare them with the typhoon wave inside theXinhai Bay of the Haikou City so to expound the difference of typhoon wave distribu-tions between bays of different geographical positions.
分析了大亚湾湾口测点儿和湾内测点W2的台风波浪资料,并与海口新海湾内测点B的波能消衰情况进行对比,说明不同地理位置海湾内的台风波浪分布特性之差异。
3.
Several important elements affecting typhoon wave calculation are clarified in this paper.
本文阐明了影响计算海湾内台风波浪的重要因素,使用我们目前已改进了的模式,可克服以往的计算缺陷,而使计算效果达到最佳。
3)  wind wave height
风浪波高
1.
The empirical relation of the wind wave height and the wind speed with steady wave at Nanji ocean station;
南麂站定常波风浪波高与风速的经验关系
4)  typhoon wave height
台风波高
1.
Taking maximum typhoon wave height series observed at Nakagusukuwan Observation Station in Japan,Poisson-maximum entropy distribution is presented to calculate typhoon wave height return values.
采用年极值法与过阈法对台风波高进行长期统计分析。
5)  typhoon wind wave
台风风浪
1.
,this article puts forth a computation method for the typhoon wind wave in shallow water regions which are affected by the coast and islands (including the bay region).
在我国港口工程技术规范的波浪成长理论基础上,考虑到台风波浪的基本特点、等效水深的概念、浅水区波浪的折射、不规则波的能量分布特性、受陆岸和岛屿影响角度范围内的有效能量风区长度等因素,提出了受陆岸、岛屿影响浅水区(包括海湾区)台风风浪的计算方案。
6)  maximum wave height estimation
首浪估算
补充资料:任凭风浪起,稳坐钓鱼台
1.见"任凭风浪起,稳坐钓鱼船"。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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