high water ordinary spring tide

简明释义

一般大潮高潮

英英释义

例句

1.The local authorities issued a warning about flooding during the upcoming high water ordinary spring tide.

当地政府对即将到来的高水普通大潮发布了洪水警告。

2.We planned our coastal hike for the afternoon to avoid the high water ordinary spring tide in the morning.

我们计划下午进行海岸徒步旅行，以避免早上的高水普通大潮。

3.During the high water ordinary spring tide, the beach was almost completely submerged.

在高水普通大潮期间，海滩几乎完全被淹没。

4.The harbor was bustling with activity during the high water ordinary spring tide as boats came and went.

在高水普通大潮期间，港口热闹非凡，船只进出频繁。

5.The fishermen waited for the high water ordinary spring tide to set out to sea, as it would provide better conditions.

渔民们等待高水普通大潮出海，因为这会提供更好的条件。

作文

Understanding the concept of tides is essential for anyone interested in marine science or coastal management. Among the various types of tides, the term high water ordinary spring tide refers to a specific condition that occurs during certain lunar phases. This phenomenon is crucial for predicting water levels and understanding the dynamics of coastal environments. Tides are primarily caused by the gravitational pull of the moon and the sun on the Earth’s oceans. As the moon orbits the Earth, its gravitational force causes the water to bulge out in the direction of the moon, resulting in high tides. Conversely, when the moon is on the opposite side of the Earth, another high tide occurs due to the centrifugal force created by the Earth-moon system. The high water ordinary spring tide, specifically, occurs during the full moon and new moon phases when the gravitational forces of both the sun and the moon align. During these times, the tidal range—the difference between high tide and low tide—is at its greatest. This means that the high water levels reached during a high water ordinary spring tide exceed those of regular high tides, making it a critical period for coastal ecosystems. For instance, many marine species rely on these higher water levels for spawning and feeding, as the increased water movement brings nutrients from deeper waters to the surface. Furthermore, understanding the timing and impact of the high water ordinary spring tide is vital for coastal communities. These areas often experience flooding during these high tides, which can lead to significant challenges for infrastructure, homes, and local economies. Coastal managers and urban planners must take these tides into account when developing strategies to mitigate flood risks and protect vulnerable areas. In addition to practical implications, the high water ordinary spring tide also has cultural significance in many societies. Coastal communities have historically relied on the rhythms of the tides for fishing, navigation, and agriculture. The predictable nature of these tides allows for effective planning and resource management. Moreover, with climate change leading to rising sea levels, the effects of high water ordinary spring tide may become even more pronounced. Higher baseline sea levels mean that the impacts of spring tides could result in more frequent and severe flooding events. Therefore, it is imperative for scientists and policymakers to monitor these tides closely and develop adaptive strategies to address potential future challenges. In conclusion, the high water ordinary spring tide is a significant natural occurrence that influences not only the physical environment but also the socio-economic fabric of coastal communities. By understanding this phenomenon, we can better appreciate the intricate relationship between humans and the ocean, and work towards sustainable solutions that honor this delicate balance.

理解潮汐的概念对任何对海洋科学或沿海管理感兴趣的人来说都是至关重要的。在各种潮汐类型中，术语高水普通大潮指的是在某些月相期间发生的特定条件。这种现象对于预测水位和理解沿海环境的动态至关重要。潮汐主要是由于月球和太阳对地球海洋的引力作用。随着月球围绕地球的轨道运动，其引力导致水向月球方向隆起，从而形成高潮。相反，当月球位于地球的另一侧时，由于地球-月球系统产生的离心力，另一个高潮也会发生。高水普通大潮特别发生在满月和新月阶段，此时太阳和月球的引力作用是对齐的。在这些时候，潮差——即高潮与低潮之间的差异——达到最大。这意味着在高水普通大潮期间达到的水位高于常规高潮，使其成为沿海生态系统的关键时期。例如，许多海洋物种依赖于这些更高的水位进行产卵和觅食，因为增加的水流将深水中的养分带到水面。此外，了解高水普通大潮的时间和影响对沿海社区至关重要。这些地区在这些高潮期间经常经历洪水，这可能给基础设施、住宅和地方经济带来重大挑战。沿海管理者和城市规划者必须在制定减轻洪水风险和保护脆弱地区的策略时考虑这些潮汐。除了实际影响外，高水普通大潮在许多社会中也具有文化意义。沿海社区历来依赖潮汐的节奏进行捕鱼、航行和农业。这些潮汐的可预测性使有效的规划和资源管理成为可能。此外，随着气候变化导致海平面上升，高水普通大潮的影响可能变得更加明显。更高的基线海平面意味着春潮的影响可能导致更频繁和严重的洪水事件。因此，科学家和政策制定者密切监测这些潮汐并制定适应策略以应对未来潜在挑战至关重要。总之，高水普通大潮是一个重要的自然现象，不仅影响物理环境，还影响沿海社区的社会经济结构。通过理解这一现象，我们可以更好地欣赏人类与海洋之间错综复杂的关系，并朝着可持续的解决方案努力，以尊重这种微妙的平衡。