inequality of tide

简明释义

潮汐不等

英英释义

例句

1.During the spring months, the inequality of tide 潮汐不等 is more pronounced, making navigation tricky.

在春季，潮汐不等 潮汐不等更加明显，使得航行变得棘手。

2.The fisherman had to adjust his schedule due to the inequality of tide 潮汐不等, which affected the fish's feeding patterns.

渔民不得不调整他的时间表，因为潮汐不等 潮汐不等影响了鱼的觅食模式。

3.Scientists study the inequality of tide 潮汐不等 to better understand coastal erosion.

科学家研究潮汐不等 潮汐不等以更好地理解海岸侵蚀。

4.Boaters should be aware of the inequality of tide 潮汐不等 when planning their trips.

船员在计划旅行时应注意潮汐不等 潮汐不等。

5.The local marina experienced issues with boat docking because of the inequality of tide 潮汐不等 during high season.

由于旺季期间的潮汐不等 潮汐不等，当地码头在船只停靠方面遇到了问题。

作文

The phenomenon of the sea's ebb and flow has fascinated humanity for centuries. Among the various aspects of this natural occurrence, the inequality of tide stands out as a particularly intriguing subject. The inequality of tide refers to the differences in tidal heights that occur due to various factors, including the position of the moon, the gravitational pull of the sun, and the geographical features of coastlines. Understanding this concept is essential for those who engage in maritime activities, such as fishing, shipping, and coastal management.Tides are primarily caused by the gravitational forces exerted by the moon and the sun on the Earth's oceans. As the moon orbits our planet, its gravitational pull creates bulges in the ocean, leading to high tides. Conversely, areas of lower water are created on the opposite side of the Earth, resulting in low tides. However, the inequality of tide arises when these tidal bulges are not uniform across different locations. For instance, some coastal regions experience significantly higher high tides and lower low tides compared to others.Several factors contribute to this inequality of tide. One major factor is the elliptical shape of the Earth's orbit around the sun, which causes variations in the distance between the Earth and the sun throughout the year. When the Earth is closest to the sun, known as perihelion, the sun's gravitational pull is stronger, resulting in higher tides. Similarly, the moon's position relative to the Earth also affects tidal patterns. When the moon is full or new, its gravitational pull aligns with that of the sun, leading to spring tides, which are characterized by exceptionally high and low tides. In contrast, during the first and third quarters of the moon, the gravitational forces partially cancel each other out, resulting in neap tides, which are less extreme.Geographical features also play a crucial role in the inequality of tide. Coastal areas with deep bays or estuaries may experience amplified tidal effects due to the funneling of water into narrower spaces. This can lead to more pronounced tidal fluctuations. Additionally, local wind patterns and atmospheric pressure can influence how water is distributed along coastlines, further contributing to the inequality of tide.For those involved in maritime industries, understanding the inequality of tide is vital for planning and operations. Fishermen must be aware of tidal patterns to optimize their catch, while shipping companies need to consider tides when scheduling arrivals and departures. Coastal engineers also rely on tidal information to design structures that can withstand the forces of changing water levels.In conclusion, the inequality of tide is a complex interplay of gravitational forces, celestial mechanics, and local geography. It highlights the dynamic nature of our planet's oceans and serves as a reminder of the intricate relationships between natural phenomena. By studying the inequality of tide, we gain valuable insights into the behavior of our seas and the impact it has on human activities. As we continue to explore and understand these natural processes, we can better prepare for the challenges and opportunities they present in our ever-changing world.

海洋的潮起潮落现象吸引了人类几个世纪的关注。在这一自然现象的各个方面中，潮汐不平衡作为一个特别引人入胜的主题脱颖而出。潮汐不平衡指的是由于各种因素造成的潮位高度差异，包括月球的位置、太阳的引力以及海岸线的地理特征。理解这一概念对于从事海洋活动的人士，如捕鱼、航运和沿海管理至关重要。潮汐主要是由于月球和太阳对地球海洋施加的引力造成的。当月球绕地球运行时，它的引力在海洋中产生隆起，导致高潮。相反，地球另一侧形成低水位区域，从而导致低潮。然而，潮汐不平衡的出现是因为这些潮汐隆起在不同地点并不均匀。例如，一些沿海地区的高潮和低潮显著高于其他地区。多种因素促成了这种潮汐不平衡。一个主要因素是地球围绕太阳的椭圆形轨道，这导致地球与太阳之间的距离在一年中发生变化。当地球靠近太阳时，即近日点，太阳的引力更强，从而导致潮位升高。类似地，月球相对于地球的位置也会影响潮汐模式。当月亮是满月或新月时，它的引力与太阳的引力对齐，导致春潮，其特点是异常高和低的潮位。相比之下，在上弦月和下弦月期间，引力部分相互抵消，导致小潮，潮位变化较小。地理特征在潮汐不平衡中也发挥着关键作用。拥有深湾或河口的沿海地区可能由于水流向狭窄空间的汇聚而经历放大的潮汐效应。这可能导致潮位波动更加明显。此外，当地的风模式和气压也会影响水在海岸线上的分布，进一步促成潮汐不平衡。对于参与海洋产业的人士而言，了解潮汐不平衡对计划和操作至关重要。渔民必须了解潮汐模式，以优化捕捞，而航运公司在安排到达和出发时需要考虑潮汐。沿海工程师还依赖潮汐信息来设计能够承受潮位变化力量的结构。总之，潮汐不平衡是引力、天体力学和地方地理之间复杂的相互作用。它凸显了我们星球海洋的动态特性，并提醒我们自然现象之间错综复杂的关系。通过研究潮汐不平衡，我们获得了关于海洋行为的宝贵见解，以及其对人类活动的影响。随着我们继续探索和理解这些自然过程，我们可以更好地为它们在不断变化的世界中带来的挑战和机遇做好准备。