mean high water neap tides

简明释义

同上

英英释义

例句

1.Understanding the mean high water neap tides 平均高水位的小潮 is crucial for coastal planning and development.

理解平均高水位的潮汐对于沿海规划和开发至关重要。

2.The construction team scheduled the work to avoid the mean high water neap tides 平均高水位的小潮 that could affect their foundation.

施工团队安排工作以避开可能影响基础的平均高水位的潮汐。

3.Boaters need to be aware of the mean high water neap tides 平均高水位的小潮 to ensure they can safely navigate the channels.

船员需要注意平均高水位的潮汐，以确保他们能够安全航行于水道。

4.During the mean high water neap tides 平均高水位的小潮, we observed a significant increase in marine life near the shore.

在平均高水位的潮汐期间，我们观察到近岸海洋生物显著增加。

5.The fisherman adjusted his nets according to the mean high water neap tides 平均高水位的小潮 to maximize his catch.

渔民根据平均高水位的潮汐调整了渔网，以最大化捕获量。

作文

Understanding tidal movements is essential for various fields, including navigation, fishing, and environmental science. One important concept in this context is mean high water neap tides, which refers to the average height of high tides during neap tide periods. Neap tides occur when the gravitational forces of the moon and sun are at right angles to each other, resulting in lower high tides and higher low tides. This phenomenon typically happens twice a month, approximately one week after the full moon and the new moon. Understanding mean high water neap tides can significantly impact coastal management and marine activities.The term mean high water neap tides encapsulates two critical aspects of tidal behavior: 'mean high water' and 'neap tides.' The 'mean high water' level is calculated by averaging the heights of high tides over a specific period, usually a lunar month. This average provides a reliable baseline for understanding tidal patterns and their variations. On the other hand, 'neap tides' are characterized by their reduced amplitude compared to spring tides, which occur when the moon and sun align, producing higher high tides and lower low tides.In practical terms, knowledge of mean high water neap tides is crucial for various activities. For instance, fishermen often rely on tidal patterns to determine the best times for fishing. During neap tides, certain fish species may be more active due to changes in water movement and availability of food. Similarly, boaters and sailors must consider these tidal variations to navigate safely, avoiding potential hazards associated with low water levels.Environmental scientists also pay close attention to mean high water neap tides as they study coastal ecosystems. Tidal fluctuations play a vital role in shaping habitats, influencing the distribution of plant and animal species. By understanding how neap tides interact with mean high water levels, researchers can assess the health of coastal environments and predict how they might respond to climate change and rising sea levels.Moreover, urban planners and coastal managers utilize data on mean high water neap tides to make informed decisions regarding land use and infrastructure development. Coastal areas are often vulnerable to flooding and erosion, especially during extreme weather events. By incorporating tidal data into their planning processes, authorities can better protect communities and preserve valuable ecosystems.In conclusion, the concept of mean high water neap tides is integral to understanding tidal dynamics and their implications for various sectors. Whether for fishing, navigation, environmental conservation, or urban planning, grasping the significance of this term allows stakeholders to make informed decisions that enhance safety, sustainability, and ecological integrity. As we continue to explore the complexities of our oceans and coastlines, the importance of understanding tidal phenomena like mean high water neap tides will only grow, highlighting the interconnectedness of natural systems and human activities.

理解潮汐运动对于导航、渔业和环境科学等多个领域至关重要。在这个背景下，一个重要的概念是平均高水位小潮，它指的是在小潮期间高水位的平均高度。小潮发生在月球和太阳的引力相互垂直时，导致高水位较低，低水位较高。这一现象通常每月发生两次，大约在满月和新月后的一周。理解平均高水位小潮对沿海管理和海洋活动具有重要影响。术语平均高水位小潮包含了潮汐行为的两个关键方面：“平均高水位”和“小潮”。“平均高水位”是通过对特定时期内高水位的高度进行平均计算得出的，通常为一个月亮周期。这个平均值提供了理解潮汐模式及其变化的可靠基线。另一方面，“小潮”则以其相较于春潮的幅度减小而著称，春潮发生在月球和太阳对齐时，产生更高的高水位和更低的低水位。在实际应用中，了解平均高水位小潮对各种活动至关重要。例如，渔民通常依赖潮汐模式来确定最佳捕鱼时间。在小潮期间，由于水流和食物供应的变化，某些鱼类可能会更加活跃。同样，船员和水手必须考虑这些潮汐变化，以安全航行，避免与低水位相关的潜在危险。环境科学家也密切关注平均高水位小潮，因为他们研究沿海生态系统。潮汐波动在塑造栖息地、影响植物和动物物种分布方面发挥着重要作用。通过理解小潮如何与平均高水位水平相互作用，研究人员可以评估沿海环境的健康状况，并预测它们如何应对气候变化和海平面上升。此外，城市规划者和沿海管理者利用平均高水位小潮的数据来就土地使用和基础设施发展做出明智的决策。沿海地区通常容易受到洪水和侵蚀的影响，尤其是在极端天气事件期间。通过将潮汐数据纳入规划过程，相关部门可以更好地保护社区并保护宝贵的生态系统。总之，平均高水位小潮的概念对理解潮汐动态及其对各个部门的影响至关重要。无论是为了捕鱼、导航、环境保护还是城市规划，掌握这一术语的意义使利益相关者能够做出增强安全性、可持续性和生态完整性的明智决策。随着我们继续探索海洋和海岸线的复杂性，理解潮汐现象如平均高水位小潮的重要性只会增加，突显出自然系统与人类活动之间的相互联系。