风海流

fēng hǎi liú
  • wind current
风海流风海流
风海流[fēng hǎi liú]
  1. 风海流对海面污油漂移路线的影响

    Impact of wind current on drift path of spillage at sea

  2. 台湾海峡风海流的数值计算

    Numerical calculation of the wind current of the Taiwan Strait

  3. 本文基于漂流理论基础方程式,应用Ritz求解变分问题的近似数值法,讨论浅海水深变化时,在海湾、航道内的风海流计算的一种近似数值解。

    Basing on the fundamental dynamic equations of drift current , this paper presents a numerical value solution to the computation of wind-driven currents in sea inlets and navigation channels with various water depths by the application of the approximate value method in terms of Ritz solution to variation .

  4. 计算陆架风海流的一种模式

    A model for calculating wind-driven ocean current on continental shelf

  5. 台湾海峡三维风海流的数值模拟

    Numerical simulation of 3D wind current in Taiwan Strait

  6. 风海流消衰理论的初步研究

    Preliminary study on the decay theory of wind-driven current

  7. 确定近岸风海流椭圆的一个简单方法

    A simple method to define offshore wind-driven current ellipse

  8. 线性倾斜陆架上的定常风海流

    Steady wind-driven sea current on linear sloping continental shelf

  9. 北太平洋风海流季节变化的数值模拟

    The seasonal variability of wind - driven currents in a model of the North Pacific

  10. 因此,作者着重对台湾海峡的潮波和风海流进行了模拟和研究。

    Accordingly , the tide wave and the wind current are studied by numerical modeling elaborately in this paper .

  11. 这些风海流可以在加勒比海制造风切,阻碍在年夜西洋的飓风度长。

    Those wind currents can create wind shear in the Caribbean , which inhibits hurricane development in the Atlantic .

  12. 渤海及黄海北部的风海流数值计算及余流计算

    A Numerical Computation of Wind-Induced Currents and Computation of Residual Currents in the Bohai Sea and the Northern Part of the Yellow Sea

  13. 当承平洋的海水比凡是暖和的时辰,厄尔尼诺现象就影响风海流。

    El Ni ? o is when some of the Pacific Ocean 's waters become warmer than normal , affecting the wind currents .

  14. 本文给出了无限水深情况下漂流运动方程的求解过程,以及风海流速度垂直分布的规律性。

    A solution process of the equation of Ekman drift motion in infinite deep sea is given in this paper . Furthermore , the regularity of vertical distribution of drift velocity is discussed .

  15. 首先分析外海流系,沿岸流系,风海流、潮流,并以数学方程式描述之,然后作半浮体漂移的推算,最后以实例验证。

    At frist , the outer sea current system , the coastal current system , the wind sea current and tide are analysed with the description of mathematical equations . Then , the drift of semi-floating body is predicted and checked with an example .

  16. 余流以风海流为主导地位,海面在西南风的作用下,海水向湾内东北部流动,海面在东风和东南风的作用下,海水向西流动,余流最大流速仅为29.3cm/s。

    Under the control of the Southwest wind , Sea water flows to the northeast in the bay . And it flows westward on the results of the east and southeast wind . The maximun velocity of residual current is only 29 . 3cm / s.

  17. 在有利的风和海流作用下,亦可横跨黄海、影响朝鲜半岛南部邻近海域。

    Macro-algae patches were also found to drift eastwardly towards the Korea Peninsular , which are supposed to be driven by the sea surface wind .

  18. 这些被模拟和预报的环境要素场,例如海面风、海流和海浪,都被用于计算船舶在该种海洋环境条件下的运动和姿态。

    At the same time , the simulated datum of wind , current and wave can be introduced into calculating the ship movement and motion in this marine environment .

  19. 受风驱动的海流也有同样的变化。

    Currents generated by the winds likewise vary .

  20. 只要输入海面气压场并利用迭代方法,即可求得海洋表面的风场和海流场。

    The sea surface winds and the ocean surface currents can be obtained by iteration method as long as the sea surface level pressure fields are input .

  21. 南海北部海面风场和平均海流场模拟

    Simulation of Wind Fields and Mean Flow Field of the North Part of South China Sea

  22. 但由于海洋平台所处的海洋环境十分复杂和恶劣,风、波浪、海流和潮汐及其他不确定载荷等各种动静载荷往往对平台结构的安全构成极大的威胁。

    However , the marine environment is very complex and harsh , wind , waves , currents and tides and other uncertainties tend to load a variety of static and dynamic loads may threaten the safety of platform .

  23. 船舶动力定位是依靠自身的动力,在控制系统的指挥下抵抗外界的干扰(风、浪和海流等),使其保持某一位置和艏向、悬停于空间任何一定点位置。

    Depending on its own power , resisting external interferences ( wind , wave and ocean current etc ) in command of control system , the fundamental goal of dynamic positioning is to keep ship steadily in given position and yaw angel .

  24. 依据黄渤海实测风的资料对渤海及北黄海进行了月平均风海流数值计算。

    Using the data of measured wind , the monthly average wind induced currents were numerically computed in the Bohai Sea and the northern part of the Yellow Sea .