mean low water neaps
简明释义
平均小潮低潮小潮低潮
英英释义
Mean Low Water Neaps refers to the average level of low water during neap tides, which occur when the difference between high and low tide is at its minimum. | 平均低潮小潮指的是在小潮期间的平均低水位,小潮发生在高潮和低潮之间的差异最小的时候。 |
例句
1.The harbor is less crowded during the mean low water neaps, making it easier for boats to dock.
在平均低水小潮期间,港口较少拥挤,使船只更容易靠岸。
2.Understanding the timing of mean low water neaps is crucial for coastal construction projects.
了解平均低水小潮的时机对沿海建设项目至关重要。
3.The tide chart indicates that the next mean low water neaps will occur next weekend.
潮汐图显示下一个平均低水小潮将在下周末发生。
4.During the mean low water neaps, we can safely explore the tidal pools along the shore.
在平均低水小潮期间,我们可以安全地探索沿海的潮池。
5.Fishermen often prefer to go out during the mean low water neaps for better access to certain fish species.
渔民通常喜欢在平均低水小潮期间出海,以便更好地接触到某些鱼类。
作文
Understanding tidal phenomena is crucial for various fields, including maritime navigation, coastal engineering, and environmental science. One of the essential concepts in this area is the term mean low water neaps, which refers to a specific point in the tidal cycle. To grasp its significance, we must first understand the basic principles of tides and their variations.Tides are caused primarily by the gravitational pull of the moon and the sun on the Earth's oceans. They result in periodic changes in sea level, which can be classified into different stages: high tide and low tide. Within these stages, there are further distinctions, particularly between spring tides and neap tides. Spring tides occur when the sun, moon, and Earth align, leading to higher high tides and lower low tides. In contrast, neap tides happen when the moon is in its first or third quarter phase, resulting in lower high tides and higher low tides.The term mean low water neaps specifically refers to the average level of water during neap tides. It represents the lowest level of water that can be expected during these periods. Understanding this measurement is vital for several reasons. For instance, it helps in predicting the availability of navigable waters for ships and boats. Knowing the mean low water neaps allows mariners to plan their journeys more effectively, avoiding grounding during low tides.Moreover, coastal engineers utilize the concept of mean low water neaps when designing structures such as docks, piers, and seawalls. By knowing the average low water level, they can ensure that these structures are built to withstand the forces of nature while remaining functional during various tidal conditions. This understanding also plays a critical role in environmental conservation efforts, as it helps scientists assess the health of coastal ecosystems and the impact of human activities on these delicate environments.Additionally, the mean low water neaps serves as a reference point for various legal and regulatory frameworks concerning land use and property rights along coastlines. In many jurisdictions, the ownership of land adjacent to water bodies is determined by the mean low water mark. Thus, having a clear understanding of what constitutes mean low water neaps can prevent disputes and clarify property boundaries.In conclusion, the concept of mean low water neaps is an integral part of understanding tidal dynamics and their implications for navigation, engineering, and environmental management. By recognizing its importance, professionals in various fields can make informed decisions that contribute to safer and more sustainable interactions with our oceans and coastlines. As we continue to study and monitor tidal patterns, the significance of terms like mean low water neaps will only grow, highlighting the intricate relationship between humans and the natural world.
理解潮汐现象对于海洋导航、沿海工程和环境科学等多个领域至关重要。在这一领域,一个重要的概念是术语平均低水小潮,它指的是潮汐周期中的一个特定点。要掌握它的意义,我们首先必须了解潮汐及其变化的基本原理。潮汐主要是由于月球和太阳对地球海洋的引力造成的。它们导致海平面的周期性变化,这些变化可以分为不同的阶段:高潮和低潮。在这些阶段中,特别是在春潮和小潮之间有进一步的区分。春潮发生在太阳、月球和地球对齐时,导致更高的高潮和更低的低潮。相反,小潮发生在月亮处于上弦或下弦相位时,导致较低的高潮和较高的低潮。术语平均低水小潮特指小潮期间的平均水位。它代表了在这些时期内可以预期的最低水位。理解这一测量值至关重要,原因有很多。例如,它有助于预测船只和船只的可航行水域的可用性。了解平均低水小潮使海员能够更有效地规划他们的航程,避免在低潮时搁浅。此外,沿海工程师在设计码头、栈桥和防波堤等结构时也利用平均低水小潮的概念。通过了解平均低水位,他们可以确保这些结构在抵御自然力量的同时保持在各种潮汐条件下的功能。这种理解在环境保护工作中也发挥着关键作用,因为它帮助科学家评估沿海生态系统的健康状况以及人类活动对这些脆弱环境的影响。此外,平均低水小潮作为涉及土地使用和沿海地产权的各种法律和监管框架的参考点。在许多法域中,邻近水体的土地所有权由平均低水线决定。因此,清楚理解什么构成平均低水小潮可以防止争端并明确财产边界。总之,平均低水小潮的概念是理解潮汐动态及其对导航、工程和环境管理影响的重要组成部分。通过认识到它的重要性,各个领域的专业人士可以做出明智的决策,从而促进与我们海洋和海岸线的更安全和可持续的互动。随着我们继续研究和监测潮汐模式,像平均低水小潮这样的术语的重要性将只会增加,突显人类与自然世界之间错综复杂的关系。