dynamictheory of tide

简明释义

潮汐动力论

英英释义

例句

1.The dynamictheory of tide explains how gravitational forces affect water levels in the ocean.

潮汐的动态理论 解释了重力如何影响海洋水位。

2.In marine biology, understanding the dynamictheory of tide is crucial for studying coastal ecosystems.

在海洋生物学中，理解 潮汐的动态理论 对研究沿海生态系统至关重要。

3.The dynamictheory of tide incorporates both lunar and solar influences on tides.

潮汐的动态理论 包括月球和太阳对潮汐的影响。

4.The dynamictheory of tide helps predict tidal patterns, which is essential for navigation.

潮汐的动态理论 有助于预测潮汐模式，这对航行至关重要。

5.Engineers use the principles of the dynamictheory of tide to design tidal energy systems.

工程师利用 潮汐的动态理论 的原理来设计潮汐能系统。

作文

The study of tides has fascinated scientists for centuries, leading to the development of various theories to explain their behavior. One of the most significant advancements in our understanding of tidal movements is the dynamictheory of tide. This theory provides a comprehensive framework for analyzing how tides are influenced not only by the gravitational pull of the moon and the sun but also by the Earth's rotation and the shape of its coastline.To understand the dynamictheory of tide, we must first recognize that tides are not merely simple oscillations of water. Instead, they are complex phenomena resulting from the interplay between gravitational forces and the dynamic characteristics of ocean water. The dynamictheory of tide considers factors such as the speed of wave propagation, the depth of the ocean, and the varying topography of the sea floor. These elements contribute to the formation of tidal waves that can have different heights and timings depending on the location.In contrast to the older static models of tides, which primarily focused on the gravitational forces acting upon bodies of water, the dynamictheory of tide incorporates the principles of fluid dynamics. This approach allows for a more accurate prediction of tidal patterns, especially in regions with complicated coastlines where water can funnel into bays or estuaries, amplifying the tidal effects.One of the key aspects of the dynamictheory of tide is the concept of resonance. Certain geographical features can cause the natural frequency of the water body to align with the frequency of the tidal forces, leading to significantly higher tides known as 'resonant tides.' For example, the Bay of Fundy in Canada is famous for having some of the highest tides in the world, largely due to its unique shape and the resonance effect.Additionally, the dynamictheory of tide explains how tidal waves can travel across vast distances. As the Earth rotates, different areas experience high and low tides at different times. This phenomenon is further complicated by the fact that tidal waves can be reflected and refracted by coastlines, creating variations in timing and height even within short distances.The implications of the dynamictheory of tide extend beyond mere academic interest. Understanding tidal dynamics is crucial for navigation, coastal management, and predicting the impacts of climate change on sea levels. For instance, rising sea levels may alter tidal patterns, affecting ecosystems and human settlements along coastlines.In conclusion, the dynamictheory of tide represents a significant leap forward in our understanding of tidal movements. By integrating the principles of fluid dynamics with gravitational influences, this theory offers a more nuanced perspective on how tides operate. As we continue to explore the complexities of our oceans, the dynamictheory of tide will undoubtedly remain a vital tool for scientists and researchers seeking to unravel the mysteries of these powerful natural forces.

潮汐的研究吸引了科学家们几个世纪以来的关注，导致了各种理论的发展，以解释其行为。我们对潮汐运动的理解中最重要的进展之一是dynamictheory of tide（潮汐动力学理论）。该理论提供了一个全面的框架，用于分析潮汐如何不仅受到月球和太阳的引力影响，还受到地球自转和海岸线形状的影响。要理解dynamictheory of tide，我们首先必须认识到潮汐不仅仅是水的简单振荡。相反，它们是复杂的现象，源于引力作用和海洋水体动态特性之间的相互作用。dynamictheory of tide考虑了波传播速度、海洋深度和海底变化的地形等因素。这些元素共同促进了潮汐波的形成，这些潮汐波的高度和时间因地点而异。与主要关注作用于水体的引力的较旧静态模型相比，dynamictheory of tide结合了流体动力学的原理。这种方法允许更准确地预测潮汐模式，特别是在海岸线复杂的地区，水可以汇聚到海湾或河口，从而放大潮汐效应。dynamictheory of tide的一个关键方面是共振的概念。某些地理特征可能导致水体的自然频率与潮汐力量的频率一致，从而导致显著更高的潮汐，称为“共振潮”。例如，加拿大的芬迪湾因其独特的形状和共振效应而以拥有世界上最高的潮汐而闻名。此外，dynamictheory of tide解释了潮汐波如何在广阔的距离上移动。随着地球的自转，不同区域在不同时间经历高潮和低潮。这一现象进一步复杂化，因为潮汐波可以被海岸线反射和折射，即使在短距离内也会导致时间和高度的变化。dynamictheory of tide的影响超出了单纯的学术兴趣。了解潮汐动态对于航海、沿海管理和预测气候变化对海平面的影响至关重要。例如，海平面上升可能改变潮汐模式，影响沿海生态系统和人类定居点。总之，dynamictheory of tide代表了我们对潮汐运动理解的重要飞跃。通过将流体动力学的原理与引力影响相结合，该理论提供了对潮汐如何运作的更细致的视角。随着我们继续探索海洋的复杂性，dynamictheory of tide无疑将继续成为科学家和研究人员揭示这些强大自然力量奥秘的重要工具。