antilunar tide

简明释义

反月潮

英英释义

例句

1.Scientists study the effects of the antilunar tide 反月潮 on coastal erosion patterns.

科学家研究反月潮对海岸侵蚀模式的影响。

2.During the full moon, the antilunar tide 反月潮 can be observed more prominently along the coast.

在满月期间，沿海地区可以更明显地观察到反月潮。

3.The oceanographer explained that the antilunar tide 反月潮 occurs when the moon is on the opposite side of the Earth.

海洋学家解释说，当月球位于地球的另一侧时，会发生反月潮。

4.The fishermen adjusted their schedules to account for the antilunar tide 反月潮 affecting fish behavior.

渔民们调整了他们的日程，以考虑到影响鱼类行为的反月潮。

5.The antilunar tide 反月潮 contributes to the overall tidal cycle experienced by coastal regions.

在沿海地区，反月潮对整体潮汐循环有贡献。

作文

The phenomenon of tides has fascinated humanity for centuries, influencing everything from navigation to coastal ecosystems. Among the various types of tides, the antilunar tide is particularly intriguing. This term refers to the tidal forces that occur on the side of the Earth opposite to the moon. While most people are familiar with the concept of high and low tides caused by the gravitational pull of the moon, the antilunar tide represents an equally important aspect of tidal dynamics that is often overlooked.Tides are primarily driven by the gravitational forces exerted by the moon and the sun. The moon's gravitational pull creates a bulge of water on the side of the Earth that faces it, resulting in what we call the 'direct tide'. However, the Earth itself is also pulled slightly toward the moon, creating a second bulge on the opposite side. This phenomenon is what we refer to as the antilunar tide. It is essential to understand that this tide is not simply a reaction to the moon's presence; it is a result of the complex interplay between gravitational forces and the Earth's rotation.The antilunar tide plays a crucial role in the overall tidal cycle. During a full moon or new moon, when the Earth, moon, and sun align, both the direct tide and the antilunar tide are at their peak, leading to exceptionally high and low tides known as spring tides. Conversely, during the first and third quarters of the moon, when the moon and sun are at right angles relative to the Earth, the effects of the antilunar tide and the direct tide partially cancel each other out, resulting in lower high tides and higher low tides, known as neap tides.Understanding the antilunar tide is not just an academic exercise; it has practical implications for coastal management and navigation. For example, fishermen and sailors must be aware of these tidal patterns to optimize their activities. Coastal ecosystems also rely on predictable tidal movements for the health of marine habitats. Organisms such as crabs, fish, and sea birds have evolved to time their breeding and feeding cycles according to these tidal rhythms, which include the influence of the antilunar tide.Moreover, the study of tides, including the antilunar tide, has broader implications in understanding climate change and its impact on sea levels. As global temperatures rise, the melting of polar ice caps and glaciers contributes to rising sea levels, which can alter tidal patterns and exacerbate coastal erosion. Therefore, researchers are increasingly focusing on how changes in tidal dynamics, including the antilunar tide, may affect coastal communities and ecosystems.In conclusion, the antilunar tide is a vital component of our planet's tidal system, representing the gravitational dance between the Earth and its celestial neighbors. By recognizing and studying this phenomenon, we can gain deeper insights into the complexities of our natural world, ensuring that we manage our coastal resources wisely and sustainably. Whether we are navigating the open seas or simply enjoying a day at the beach, the effects of the antilunar tide are all around us, reminding us of the intricate connections that bind us to the cosmos.

潮汐现象数百年来一直吸引着人类的注意，影响着从航海到沿海生态系统的方方面面。在各种潮汐类型中，反月潮尤其引人入胜。这个术语指的是发生在地球与月球相对一侧的潮汐力量。虽然大多数人熟悉因月球的引力造成的高潮和低潮的概念，但反月潮代表了潮汐动态中一个同样重要但常被忽视的方面。潮汐主要是由月球和太阳施加的引力驱动的。月球的引力在面对它的地球一侧形成水的隆起，产生我们称之为“直接潮”。然而，地球本身也会略微向月球移动，造成另一侧的隆起。这种现象就是我们所称的反月潮。必须理解，这种潮汐不仅仅是对月球存在的反应；它是引力作用与地球自转之间复杂相互作用的结果。反月潮在整体潮汐周期中扮演着至关重要的角色。在满月或新月期间，当地球、月球和太阳排成一线时，直接潮和反月潮都达到峰值，导致异常高和低的潮汐，称为春潮。相反，在上弦月和下弦月期间，当月球和太阳相对于地球呈直角时，反月潮和直接潮的影响部分相互抵消，导致较低的高潮和较高的低潮，称为死潮。了解反月潮不仅仅是学术研究，它对沿海管理和航海有实际意义。例如，渔民和水手必须了解这些潮汐模式，以优化他们的活动。沿海生态系统也依赖于可预测的潮汐运动来维持海洋栖息地的健康。螃蟹、鱼类和海鸟等生物已经进化出根据这些潮汐节律（包括反月潮的影响）来安排繁殖和觅食周期。此外，对潮汐的研究，包括反月潮，在理解气候变化及其对海平面的影响方面具有更广泛的意义。随着全球温度上升，极地冰盖和冰川的融化导致海平面上升，这可能改变潮汐模式，加剧沿海侵蚀。因此，研究人员越来越关注潮汐动态变化，包括反月潮，可能如何影响沿海社区和生态系统。总之，反月潮是我们星球潮汐系统的重要组成部分，代表了地球与其天体邻居之间的引力舞蹈。通过认识和研究这一现象，我们可以深入了解我们自然世界的复杂性，确保我们明智和可持续地管理我们的沿海资源。无论我们是在开放海域航行，还是仅仅享受海滩的一天，反月潮的影响无处不在，提醒我们联系宇宙的复杂关系。