resultant tide

简明释义

合成潮

英英释义

例句

1.The coastal engineers studied the effect of the moon's position on the resultant tide 结果潮 to better predict flooding.

沿海工程师研究了月亮位置对结果潮 结果潮的影响，以更好地预测洪水。

2.Scientists measured the resultant tide 结果潮 to understand its impact on marine life.

科学家测量了结果潮 结果潮以了解其对海洋生物的影响。

3.During the storm, the resultant tide 结果潮 caused significant erosion along the beach.

在风暴期间，结果潮 结果潮导致海滩严重侵蚀。

4.The fishermen adjusted their schedules based on the predicted resultant tide 结果潮 for optimal catch.

渔民根据预测的结果潮 结果潮调整了他们的作业时间，以获得最佳捕捞。

5.Understanding the resultant tide 结果潮 is crucial for navigation in shallow waters.

理解结果潮 结果潮对于在浅水区导航至关重要。

作文

The ocean is a vast and mysterious entity, constantly influenced by numerous factors. One of the most significant influences on oceanic movements is the gravitational pull of the moon and the sun, which leads to the phenomenon known as tides. Among the various types of tides, the resultant tide 合成潮 plays a crucial role in understanding how these forces interact to create the ebb and flow of the sea. The resultant tide 合成潮 can be defined as the net effect of all the tidal forces acting upon a body of water at a given time. It is not merely the sum of the individual contributions from the moon and the sun; instead, it represents the complex interplay between these celestial bodies and the Earth’s rotation. This interaction leads to varying tidal patterns that can differ significantly from one location to another.To grasp the concept of the resultant tide 合成潮, one must first understand the two primary components that contribute to it: the lunar tide and the solar tide. The lunar tide is primarily caused by the moon’s gravitational force pulling on the Earth’s oceans. As the moon orbits the Earth, it creates bulges in the water, leading to high tides. Conversely, when the moon is on the opposite side of the Earth, low tides occur as the water is pulled away from that area.On the other hand, the solar tide is influenced by the sun’s gravity. Although the sun is much larger than the moon, it is also much farther away, which makes its gravitational influence less pronounced. However, during specific alignments, such as during full moons or new moons, the solar tide can combine with the lunar tide to create exceptionally high or low tides, known as spring tides.The resultant tide 合成潮 is thus a combination of these two forces, taking into account their relative positions and the Earth’s rotation. In some locations, the resultant tide 合成潮 may result in larger tidal ranges, while in others, it may lead to minimal changes in water levels. This variability can have significant implications for coastal ecosystems, navigation, and human activities such as fishing and boating.Understanding the resultant tide 合成潮 is essential for predicting tidal patterns and their effects on marine life. For instance, many species of fish and crustaceans rely on specific tidal conditions for spawning and feeding. By studying the resultant tide 合成潮, scientists can better predict when these events will occur, allowing for more effective conservation efforts and sustainable fishing practices.In conclusion, the resultant tide 合成潮 is a fundamental concept in oceanography that illustrates the complex interactions between celestial bodies and the Earth’s waters. By understanding this phenomenon, we gain insight into the rhythms of the ocean and the delicate balance of marine ecosystems. As we continue to explore and study our oceans, the knowledge of the resultant tide 合成潮 will remain a critical component of our understanding of the natural world.

海洋是一个广阔而神秘的实体，不断受到众多因素的影响。其中，对海洋运动影响最显著的因素之一就是月球和太阳的引力，这导致了潮汐现象的出现。在各种类型的潮汐中，resultant tide 合成潮 在理解这些力量如何相互作用以创造海洋的涨落方面发挥着关键作用。resultant tide 合成潮 可以定义为在特定时间作用于水体的所有潮汐力量的净效应。它不仅仅是来自月球和太阳的个体贡献之和；相反，它代表了这些天体与地球自转之间复杂的相互作用。这种相互作用导致了不同的潮汐模式，这些模式在不同地点可能有显著差异。要理解resultant tide 合成潮 的概念，首先必须了解两个主要组成部分：月潮和日潮。月潮主要是由于月球的引力作用于地球的海洋。当月球绕地球旋转时，它会在水面上形成隆起，导致高潮。相反，当月球位于地球的另一侧时，由于水被拉走，出现低潮。另一方面，日潮则受到太阳引力的影响。尽管太阳比月球大得多，但由于距离较远，其引力影响较小。然而，在特定的对齐情况下，例如满月或新月期间，日潮可以与月潮结合，形成异常高或低的潮汐，称为春潮。因此，resultant tide 合成潮 是这两种力量的结合，考虑到它们的相对位置和地球的自转。在某些地方，resultant tide 合成潮 可能导致更大的潮差，而在其他地方，可能导致水位变化很小。这种可变性对沿海生态系统、航行以及钓鱼和划船等人类活动具有重要影响。理解resultant tide 合成潮 对于预测潮汐模式及其对海洋生物的影响至关重要。例如，许多鱼类和甲壳类动物依赖特定的潮汐条件进行产卵和觅食。通过研究resultant tide 合成潮，科学家能够更好地预测这些事件何时发生，从而允许更有效的保护工作和可持续的捕捞实践。总之，resultant tide 合成潮 是海洋学中的一个基本概念，它说明了天体与地球水体之间复杂的相互作用。通过理解这一现象，我们获得了对海洋节奏和海洋生态系统微妙平衡的洞察。随着我们继续探索和研究我们的海洋，resultant tide 合成潮 的知识将始终是我们理解自然世界的关键组成部分。