mean high water neaps

简明释义

平均小潮高潮

英英释义

Mean high water neaps refers to the average height of water during neap tides, which occur when the gravitational forces of the moon and sun are perpendicular to each other, resulting in lower high tides and higher low tides.

平均高水低潮是指在低潮期间水位的平均高度,低潮发生在月球和太阳的引力相互垂直时,导致高水位较低而低水位较高。

例句

1.Navigators must take into account the mean high water neaps when charting their courses.

航海者在绘制航线时必须考虑mean high water neaps

2.The environmental study focused on the effects of erosion at the mean high water neaps line.

环境研究集中在mean high water neaps线的侵蚀影响上。

3.The coastal engineer used the term mean high water neaps to define the average height of the tide during the lowest spring tides.

海岸工程师使用术语mean high water neaps来定义最低大潮期间潮水的平均高度。

4.The construction of the seawall was based on the mean high water neaps measurements.

海堤的建设是基于mean high water neaps的测量数据。

5.When planning the marina, they had to consider the mean high water neaps to ensure boats would not be stranded at low tide.

在规划码头时,他们必须考虑mean high water neaps,以确保船只在低潮时不会搁浅。

作文

Understanding tidal measurements is crucial for various maritime activities, including navigation, fishing, and coastal management. One such measurement that often comes up in discussions of tides is mean high water neaps. This term refers to the average height of water during neap tides, which occur when the gravitational forces of the moon and the sun are at right angles to each other. During these times, the difference between high and low tide is at its minimum, resulting in lower high tides compared to spring tides.To fully grasp the significance of mean high water neaps, it is essential to understand the context in which it is used. Tides are influenced by the moon's phases, and they can be categorized into two main types: spring tides and neap tides. Spring tides occur when the sun, moon, and Earth are aligned, leading to higher high tides and lower low tides. In contrast, neap tides occur roughly twice a month, during the first and third quarters of the moon, when the sun and moon are at right angles relative to Earth.The mean high water neaps level is particularly important for fishermen and boaters. By knowing the average height of water during neap tides, they can better plan their activities, ensuring they avoid shallow areas that could lead to grounding or damage to vessels. Coastal engineers also use this measurement when designing structures like piers and jetties, as understanding the tidal range can inform decisions about construction materials and methods.Additionally, environmental scientists monitor mean high water neaps to study the impacts of climate change on sea levels and coastal ecosystems. With rising sea levels, the traditional measurements of high and low tides may shift, affecting habitats and human activities alike. By analyzing trends in tidal data, researchers can make predictions about future changes and advise policymakers on necessary adaptations.In conclusion, mean high water neaps is more than just a technical term; it plays a vital role in various fields related to marine and coastal activities. Understanding this concept helps individuals and organizations make informed decisions, whether they are navigating the waters, conducting research, or planning infrastructure. As we continue to face challenges related to climate change and rising sea levels, the importance of accurate tidal measurements will only grow, making terms like mean high water neaps increasingly relevant in our discussions about the future of our oceans and coastlines.

理解潮汐测量对于各种海洋活动至关重要,包括航行、捕鱼和沿海管理。其中一个常常出现在潮汐讨论中的测量是平均高水位小潮。这个术语指的是在小潮期间的水平均高度,小潮发生在月球和太阳的引力相互垂直时。在这些时候,高潮和低潮之间的差异达到最低点,导致与大潮相比,高潮较低。为了充分理解平均高水位小潮的意义,必须理解它使用的背景。潮汐受月相的影响,可以分为两种主要类型:大潮和小潮。大潮发生在太阳、月球和地球对齐时,导致更高的高潮和更低的低潮。相反,小潮大约每月发生两次,在新月和满月期间,太阳和月球相对于地球处于直角。平均高水位小潮水平对于渔民和船员特别重要。通过了解小潮期间水的平均高度,他们可以更好地计划活动,确保避免可能导致搁浅或损坏船只的浅水区。沿海工程师在设计码头和防波堤等结构时也会使用这一测量,因为了解潮差可以为施工材料和方法的选择提供信息。此外,环境科学家监测平均高水位小潮以研究气候变化对海平面和沿海生态系统的影响。随着海平面的上升,传统的高潮和低潮测量可能会发生变化,影响栖息地和人类活动。通过分析潮汐数据的趋势,研究人员可以预测未来的变化,并向决策者提供必要的适应建议。总之,平均高水位小潮不仅仅是一个技术术语;它在与海洋和沿海活动相关的各个领域中发挥着至关重要的作用。理解这一概念有助于个人和组织做出明智的决策,无论是航行、水域研究还是基础设施规划。随着我们继续面临与气候变化和海平面上升相关的挑战,准确的潮汐测量的重要性只会增加,使得像平均高水位小潮这样的术语在我们讨论海洋和海岸线的未来时变得越来越相关。