high water ordinary neap tide

简明释义

一般小潮高潮小潮平均高潮一般小潮高潮

英英释义

例句

1.The high water ordinary neap tide can affect the navigation of smaller vessels in the harbor.

在港口，高水位普通小潮会影响小型船只的航行。

2.The fishermen planned their trip around the high water ordinary neap tide to ensure they would catch more fish.

渔民们围绕高水位普通小潮计划他们的出行，以确保能捕到更多的鱼。

3.During the high water ordinary neap tide, we noticed that the beach was almost completely submerged.

在高水位普通小潮期间，我们注意到海滩几乎完全被淹没。

4.It's important to check the high water ordinary neap tide schedule before launching the boat.

在发船之前，查看高水位普通小潮的时间表是很重要的。

5.We experienced a beautiful view of the coastline during the high water ordinary neap tide.

在高水位普通小潮期间，我们欣赏到了海岸线的美丽景色。

作文

The study of tides is a fascinating aspect of oceanography that has significant implications for navigation, coastal management, and understanding marine ecosystems. Among the various tidal phenomena, the term high water ordinary neap tide refers to a specific type of tide that occurs during the lunar cycle. To comprehend this concept fully, it is essential to break down its components and understand their significance in the context of tidal movements.Tides are primarily caused by the gravitational pull of the moon and the sun on the Earth’s oceans. The cycle of high and low tides is influenced by the relative positions of these celestial bodies. During a full moon or a new moon, the gravitational forces align, resulting in what is known as spring tides, where the difference between high and low water levels is at its maximum. Conversely, during the first and third quarters of the moon, the gravitational forces are at right angles to each other, leading to lower tidal ranges known as neap tides.The term high water ordinary neap tide specifically describes the highest point of water level reached during a neap tide. This phenomenon occurs when the sun and moon are positioned in such a way that their gravitational effects partially cancel each other out, resulting in less pronounced tidal changes. While the term 'ordinary' suggests a regular occurrence, it is important to note that neap tides happen approximately twice a month, making them a routine part of the lunar cycle.Understanding high water ordinary neap tide is crucial for various practical applications. For instance, fishermen often rely on knowing the timing of tides to optimize their catch. Certain species of fish are more active during specific tidal phases, and understanding when these neap tides occur can enhance fishing success. Additionally, coastal communities must be aware of tidal patterns to prepare for potential flooding or erosion, especially during storms when high water levels can exacerbate damage.In terms of environmental impact, the high water ordinary neap tide plays a role in nutrient distribution within marine ecosystems. During neap tides, the reduced movement of water can lead to stagnation in certain areas, affecting the distribution of nutrients and the overall health of marine habitats. This aspect highlights the interconnectedness of tidal movements and ecological balance, underscoring the importance of monitoring tidal patterns for conservation efforts.In conclusion, the term high water ordinary neap tide encapsulates a specific aspect of tidal behavior that is essential for various fields, from fishing to environmental science. By understanding the dynamics of tides and their impacts, we can better appreciate the complexity of our planet's systems and the intricate relationships between celestial mechanics and terrestrial phenomena. As we continue to study and monitor these natural events, we can develop more effective strategies for managing our coastal resources and protecting our marine environments.

潮汐研究是海洋学中一个迷人的领域，对航海、沿海管理以及理解海洋生态系统有着重要的影响。在各种潮汐现象中，术语高水普通小潮指的是在月相周期中发生的一种特定潮汐类型。要全面理解这一概念，有必要分解其组成部分，并了解它们在潮汐运动中的重要性。潮汐主要是由于月球和太阳对地球海洋的引力作用而产生的。高潮和低潮的循环受到这些天体相对位置的影响。在满月或新月期间，引力作用相互对齐，导致所谓的春潮，即高水位和低水位之间的差异达到最大。相反，在农历的第一和第三个季度，重力作用呈直角排列，导致潮汐范围较小，称为小潮。术语高水普通小潮专门描述在小潮期间达到的水位最高点。这一现象发生在太阳和月亮以某种方式定位时，它们的引力效应部分相互抵消，从而导致潮汐变化不明显。虽然“普通”一词暗示着一种常规发生，但需要注意的是，小潮大约每月发生两次，使其成为月相周期的例行部分。理解高水普通小潮对于各种实际应用至关重要。例如，渔民通常依靠潮汐时间来优化捕捞。某些鱼类在特定潮汐阶段更为活跃，了解这些小潮发生的时间可以提高捕鱼成功率。此外，沿海社区必须意识到潮汐模式，以便为潜在的洪水或侵蚀做好准备，尤其是在暴风雨期间，高水位可能加剧损害。在环境影响方面，高水普通小潮在海洋生态系统中起着营养分布的作用。在小潮期间，水流减少可能导致某些区域的停滞，影响营养物质的分布和海洋栖息地的整体健康。这一方面强调了潮汐运动与生态平衡之间的相互联系，突显了监测潮汐模式对保护工作的必要性。总之，术语高水普通小潮概括了一种潮汐行为的特定方面，这对渔业、环境科学等多个领域至关重要。通过理解潮汐的动态及其影响，我们可以更好地欣赏我们星球系统的复杂性，以及天体力学与地球现象之间的复杂关系。随着我们继续研究和监测这些自然事件，我们可以制定更有效的策略来管理我们的沿海资源和保护我们的海洋环境。