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strong tide
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  强潮
     The general layout, structural pattern of wharf in the strong tide and torrent area of Qiantangjiang are introduced in the paper and the measures taken for the project and intimate knowledge about the design are also introduced in it.
     简要介绍了钱塘江强潮快流地区码头的平面布置、结构型式、所采取的工程措施及设计体会。
短句来源
     The abnormal distribution of high values of H(S) and its reversed gradient in this dis-trict has no relation to some environmental factors, such as salinity, depth and temperature,but is related to special dynamic factors,such as strong tide,storm surge and confluence beltof tidal currents from different directions.
     本区某些H(S)高值的异常分布及逆向梯度分布,可与环境的盐度、深度、温度因子无关,而与强潮、风暴潮以及不同方向的潮流汇合带等特殊动力因子有关。
短句来源
     Effects of the reclamation projects on hydrodynamic environment in a strong tide estuary
     强潮河口围海工程对水动力环境的影响
短句来源
     Technology of groin building against the strong tide in Qiantang Estuary
     钱塘江强潮河段修建护岸丁坝技术探讨
短句来源
     Analysis of the calculated value reveals some peculiar characteristics of tidal flow in estuaries of strong tide as in Qiantang Estuary which are somewhat different from that in other estuaries.
     分析计算结果,可以揭示出像钱塘江这样的强潮河口的一些不同于其他河口的特殊潮流特性。
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  强潮汐
     The relationship between El Nino, strong tide and volcano eruption in Ying Island in Japan
     厄尔尼诺事件和强潮汐与日本樱岛火山爆发的对应关系
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  “strong tide”译为未确定词的双语例句
     Proportion design of corrosion resisting high-grade concrete for strong tide
     强感潮河段耐蚀性高标号混凝土配合比设计
短句来源
     The new technology of T、shaped dike made with piles was successfully used in the strong tide region in Haining country, that is a breakthrough of seawall construction technology.
     桩式丁坝新工艺、新技术在强涌潮作用的海宁段海塘塘脚的成功应用,使海塘建设技术有新的突破。
短句来源
     In the implementation of the plan, attention should be paid on ecological and environmental impact of engineering construction, meanwhile strengthening legal respect of estuary management, emergency plan for the defense of typhoon and strong tide, as well as plan for prevention of above-standard flood and typhoon disasters, so that safety of people's life and property are being secured.
     在规划实施过程中,要注意工程建设对生态与环境的影响,同时应加强河口法制化管理,做好防洪、防台风暴潮的应急抢险预案以及预防超标准洪水和台风灾害的预案工作,确保人民群众生命财产安全。
短句来源
     To meet the great trend of financial liberalization, globalization, multiple-management and net-operating, and to improve the international competitive capacity of banking service, a strong tide of mergence in the banking field has been striking the world since the mid 90s’ of 20th century, which is followed by new ones. “Super-giant bank ” comes into being one by one.
     为了适应金融自由化、全球化、综合化、网络化的大趋势,提升银行的国际竞争力,20世纪90年代中期以来,一股银行业的合并浪潮席卷国际银行界,并不断掀起新的高潮,一个个“超大银行”应运而生。
短句来源
     The results show that M 2 tidal waves in the sea area around Taiwan Strait Island are formed by tide invasion from the Pacific Ocean. and Taiwan Strait is a strong tide area;
     结果表明 ,环台湾岛海域的 M2 潮波主要为大洋传来的胁振潮 ,台湾海峡为强潮区 ;
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  strong tide
Using a vertically two-dimensional, two-layer model, we have analytically examined the generation mechanism of a nonzero Eulerian residual flow by strong tide-topography interaction in a narrow channel where the frictional effect is not included.
      
The main focus of this paper is on what strategies educational institutions in Hong Kong and China have employed in response to the strong tide of marketisation.
      
Small sailboats bucking a strong tide can have trouble just getting back through the Golden Gate.
      
Small sailboats bucking a strong tide can have trouble just getting back in through the Golden Gate.
      


There are always wide tidal flats in most estuaries,especially in Qiantang Estuary.The velocity and the rate of discharge in mainstream and tidal fiats are different from each other. In this article,the discharges as well as water levels of the mainstream and tidal flats in the same section are treated separately with full equations of motion,and the transverse excha- nge of water flow between them is also taken into account. The calculated discharge hydrographs in the mainstream and tidal fiats in two sections...

There are always wide tidal flats in most estuaries,especially in Qiantang Estuary.The velocity and the rate of discharge in mainstream and tidal fiats are different from each other. In this article,the discharges as well as water levels of the mainstream and tidal flats in the same section are treated separately with full equations of motion,and the transverse excha- nge of water flow between them is also taken into account. The calculated discharge hydrographs in the mainstream and tidal fiats in two sections of Qiantang Estuary for twelve successive tides are in good agreement with the measured value.Analysis of the calculated value reveals some peculiar characteristics of tidal flow in estuaries of strong tide as in Qiantang Estuary which are somewhat different from that in other estuaries.

大多数河口特别是钱塘江河口,往往存在宽广的潮滩地。主槽及滩地上的流速及流量不尽相同。本文将同一断面处主槽及边滩的流量及水位用各自的动量方程分开进行计算,同时也考虑了横向的水流交换。钱塘江二个断面的主槽及边滩十二个连续潮的流量过程线计算值与实测值符合甚佳。分析计算结果,可以揭示出像钱塘江这样的强潮河口的一些不同于其他河口的特殊潮流特性。

The Yangtze River Estuary is an estuary with large amount of runoff and strong tide. The average discharge of the Yangtze River is only 29,400 m3/s, while the average discharge of flood tide may get to 227,400 m3/s. The amount of sediment is about 483 million tons/yr. The dynamic interaction of these two strong forces leads to form the Yangtze River Estuary. According to the regional geological and geomorphological characteristics and their effects on heavy minerals of sediment, the source...

The Yangtze River Estuary is an estuary with large amount of runoff and strong tide. The average discharge of the Yangtze River is only 29,400 m3/s, while the average discharge of flood tide may get to 227,400 m3/s. The amount of sediment is about 483 million tons/yr. The dynamic interaction of these two strong forces leads to form the Yangtze River Estuary. According to the regional geological and geomorphological characteristics and their effects on heavy minerals of sediment, the source of the sediment at the Yangtze River Estuary can be considered as coming from 3 supplying regions, namely, the Yangtze River upstream(x1),the abandoned delta of the Yellow River at the north of Jiangsu Province (x2) and the Hangzhou Bay (x3). The converging region is the Yangtze River Estuary (y). Sampling stations are set up in the supplying regions and the converging region. According to the statistics of heavy minerals of nearly 20,000 grains of sediment collected during geological and geomorphological investigations, the author holds that heavy mineralogical characters of sediment of the Yangtze River Estuary are governed by the geological and geomorphological conditions of the watershed. According to the principle of equilibrium of sediment load, equations of the heavy mineralogical classification are presented.By means of Least Squares Method, a normal equation for calculating the converging percentages from all the supplying regions is given below:Where are the coefficients related toheavy minerals. The result shows that 96.1% of the sediment comes from the Yangtze River upstream, 7.0% from the abandoned delta of the Yellow River and-3.1% from the Hangzhou Bay.When the converging percentage of sediment from the Yangtze River upstream is known, and the total amount of sediment at Datong station is also known as 483 million tons per year, the amount of sediment at the Yangtze River Estuary (d>0.01mm) is computed, which is 359 million tons per year. This value agrees quite well with the value of 349.4 million tons per year calculated from the topographic maps of 1915 and 1963 of the Yangtze River Estuary.

根据长江口及其补给区的大量泥沙的重矿物鉴定表明,沙样中重矿含量百分数较为稳定,故能用矿物分析法计算出长江口泥沙(d>0.01毫米)的来源与数量.计算表明有96.1%来自长江补给区.据长江大通站多年平均的年输沙量推算,长江口的泥沙量为3.590亿吨/年.经1915年和1963年的长江口实测地形图比较量算的验证,两者相差2.7%.本研究法对于河口无泥沙测验与地形测量资料的情况下,研究泥沙来源与数量具有理论与实际的意义.

The evolution of tide wave near the sensible tide zone along the lower reach of the Min River has been proceeding under the condition of strong tide and strong run-off along the complex river valley. According to values of (H_K_1+H_(01))/(H_M_2) which is to the extent of 0.251—0.169, the tidal property near the sensible tide zone belongs to regular semidiurnal tide. But from the outside Min River estuary to inside, shallow water constituents MS_4, M_4 and M_6 have continually been grown...

The evolution of tide wave near the sensible tide zone along the lower reach of the Min River has been proceeding under the condition of strong tide and strong run-off along the complex river valley. According to values of (H_K_1+H_(01))/(H_M_2) which is to the extent of 0.251—0.169, the tidal property near the sensible tide zone belongs to regular semidiurnal tide. But from the outside Min River estuary to inside, shallow water constituents MS_4, M_4 and M_6 have continually been grown and become non-regular shallow semidiurnal tide. The estuary has got the characters of standing waves. The process of ebb and flow is mainly composed of flood tide——flood current and ebb tide——ebb current. During the process of going upward, the wave front of the estuary becomes steeper while the back becomes more gentle and the interval between high water and low water becomes larger. Further more the shape of the high water line becomes the shape of a saddle, the tidal range and the tidal wave's speed becomes less.

闽江感潮段潮波是在强潮、强径流及河谷形态复杂的情况下演变的。■比值在0.251—0.169范围内,属于正规半日潮,但由河口向上游,浅水分潮MS_4、M_4、M_0不断增大,成为非正规半日浅海潮。潮波具有驻波性质,涨落潮过程基本上只有涨潮—涨潮流和落潮—落潮流。由口外向口内演进过程中,潮波前坡变陡后坡变缓,高(低)潮间隙不断增大,高潮线呈马鞍形,潮差和潮波传播速度不断变小。

 
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