equilibrium tide

简明释义

天文潮汐(受日月吸力影响的潮汐

英英释义

例句

1.The equilibrium tide theory helps in understanding tidal patterns around the world.

平衡潮理论有助于理解全球潮汐模式。

2.The concept of equilibrium tide is essential for understanding oceanography.

理解海洋学时，平衡潮的概念至关重要。

3.During a full moon, the equilibrium tide can cause significantly higher sea levels.

在满月期间，平衡潮可能导致海平面显著上升。

4.Changes in atmospheric pressure can influence the equilibrium tide observed at coastal areas.

大气压力的变化会影响沿海地区观察到的平衡潮。

5.Scientists use models to predict the behavior of equilibrium tide under various conditions.

科学家使用模型预测在不同条件下的平衡潮行为。

作文

The concept of tides has fascinated humanity for centuries, influencing navigation, fishing, and even the design of coastal cities. Among the various types of tides, the equilibrium tide (平衡潮) stands out as a theoretical model that helps us understand the fundamental forces at play in the ocean. In essence, the equilibrium tide (平衡潮) refers to the idealized tidal patterns that would occur if the Earth were covered entirely by water and if there were no other influences such as landmasses or atmospheric conditions. This model assumes that the gravitational pull of the Moon and the Sun are the primary forces driving the tides, creating bulges in the ocean that result in high and low tides. Understanding the equilibrium tide (平衡潮) is crucial for both scientists and laypeople alike. It serves as a baseline from which we can analyze real-world tidal behaviors. For instance, in coastal areas where land interferes with the flow of water, actual tides may vary significantly from the predictions made by the equilibrium tide (平衡潮) model. These variations can be attributed to factors such as local geography, weather conditions, and human activities. One of the most interesting aspects of the equilibrium tide (平衡潮) is its relationship with the lunar cycle. The gravitational force exerted by the Moon causes a noticeable rise and fall in sea levels, leading to the familiar pattern of high and low tides. During a full moon or new moon, when the Earth, Moon, and Sun are aligned, we experience what are known as spring tides—higher high tides and lower low tides. Conversely, during the first and third quarters of the moon, when the Moon is at a right angle to the Sun relative to the Earth, we experience neap tides, which are less extreme. In addition to lunar influences, the equilibrium tide (平衡潮) model also considers the Sun's gravitational pull, although it is less significant than that of the Moon. The combined effects of these celestial bodies create a complex system of tidal forces that vary depending on the time of year and geographic location. For example, during certain seasons, the Sun's position can enhance or diminish the effect of the Moon's gravitational pull, leading to variations in tidal ranges. Furthermore, understanding the equilibrium tide (平衡潮) is not just an academic exercise; it has practical implications for various industries. For fishermen, knowing the timing of tides can mean the difference between a fruitful catch and an empty net. For coastal engineers, understanding tidal patterns is essential for designing structures that can withstand the forces of nature. Even for recreational boaters, knowledge of tides can enhance safety and enjoyment on the water. In conclusion, the equilibrium tide (平衡潮) serves as a foundational concept in our understanding of oceanic tides. While it is a simplified model that does not account for all variables, it provides valuable insights into the gravitational forces that shape our oceans. By studying the equilibrium tide (平衡潮) and its implications, we can better appreciate the dynamic systems that govern our planet's waters and make informed decisions in various aspects of life, from environmental conservation to economic activities. As we continue to explore the complexities of our natural world, the equilibrium tide (平衡潮) will undoubtedly remain a key element in our quest for knowledge.

潮汐的概念几个世纪以来一直吸引着人类，影响着航海、渔业，甚至沿海城市的设计。在各种潮汐类型中，equilibrium tide（平衡潮）作为一个理论模型，帮助我们理解海洋中起作用的基本力量，显得尤为突出。equilibrium tide（平衡潮）本质上指的是如果地球完全被水覆盖，并且没有其他影响，如陆地或大气条件，那么将会发生的理想潮汐模式。这个模型假设月球和太阳的引力是驱动潮汐的主要力量，造成海洋中的隆起，从而导致高潮和低潮。理解equilibrium tide（平衡潮）对科学家和普通人来说都至关重要。它作为一个基准，使我们能够分析现实世界中的潮汐行为。例如，在陆地干扰水流的沿海地区，实际潮汐可能与equilibrium tide（平衡潮）模型的预测有显著差异。这些变化可以归因于局部地理、天气条件和人类活动等因素。equilibrium tide（平衡潮）最有趣的方面之一是它与月相周期的关系。月球施加的引力导致海平面的明显升降，形成我们熟悉的高潮和低潮模式。在满月或新月期间，当地球、月球和太阳排成一线时，我们经历的称为春潮——更高的高潮和更低的低潮。相反，在月亮处于与太阳相对地球的直角位置时，即在第一和第三季度，我们会经历潮差较小的死潮。除了月球的影响外，equilibrium tide（平衡潮）模型还考虑了太阳的引力，尽管它的影响不如月球显著。这些天体的综合效应创造了一个复杂的潮汐力系统，随着季节和地理位置的不同而变化。例如，在某些季节，太阳的位置可以增强或减弱月球引力的影响，从而导致潮汐范围的变化。此外，理解equilibrium tide（平衡潮）不仅仅是学术练习；它对各个行业都有实际意义。对于渔民而言，了解潮汐的时间可能意味着丰收和空网之间的区别。对于沿海工程师来说，理解潮汐模式对设计能够抵御自然力量的结构至关重要。即使对于休闲船员来说，了解潮汐也能增强在水上的安全性和乐趣。总之，equilibrium tide（平衡潮）作为我们理解海洋潮汐的基础概念。虽然它是一个简化的模型，没有考虑所有变量，但它提供了对塑造我们海洋的引力的宝贵见解。通过研究equilibrium tide（平衡潮）及其影响，我们可以更好地欣赏支配我们星球水域的动态系统，并在生活的各个方面做出明智的决策，从环境保护到经济活动。随着我们继续探索自然世界的复杂性，equilibrium tide（平衡潮）无疑将继续成为我们追求知识的关键元素。