retardation of tide

简明释义

潮汐迟滞差

英英释义

例句

1.The retardation of tide during storms can lead to unexpected flooding in low-lying areas.

暴风雨期间的潮汐延迟可能导致低洼地区意外洪水。

2.Understanding the retardation of tide is crucial for navigation in coastal waters.

理解潮汐延迟对沿海水域的航行至关重要。

3.The engineer explained the retardation of tide in the harbor, which affects local fishing activities.

工程师解释了港口的潮汐延迟，这影响了当地的捕鱼活动。

4.Scientists are studying the retardation of tide to predict its impact on coastal erosion.

科学家正在研究潮汐延迟以预测其对海岸侵蚀的影响。

5.The retardation of tide can cause delays in ferry schedules.

潮汐的延迟可能会导致渡轮时间表的延误。

作文

The phenomenon of the retardation of tide is a fascinating aspect of oceanography that has significant implications for coastal ecosystems and human activities. Tides, which are primarily caused by the gravitational pull of the moon and the sun, exhibit a cyclical pattern of rising and falling water levels. However, various factors can influence this natural rhythm, leading to the retardation of tide or delays in the timing and height of tidal movements.One of the primary causes of the retardation of tide is the interaction between the ocean and the land. As tides approach coastal areas, they encounter friction with the seabed and the shoreline. This friction slows down the movement of water, causing a delay in the peak of the tide compared to its predicted time based on astronomical calculations. This phenomenon is particularly evident in shallow waters where the bottom topography significantly affects tidal behavior.Another factor contributing to the retardation of tide is the presence of large bodies of water, such as bays and estuaries. These areas can trap water, causing it to rise and fall at different rates than the open ocean. For instance, when high tide occurs in a bay, the water may take longer to reach its highest point due to the constricted flow of water into the narrower spaces. Similarly, during low tide, the water may recede more slowly, leading to a noticeable lag in tidal patterns.Weather conditions also play a crucial role in the retardation of tide. Storms, wind patterns, and atmospheric pressure changes can all affect tidal movements. For example, strong winds can push water towards the shore, causing a temporary increase in water levels, while low atmospheric pressure can allow water to rise more easily. These variations can lead to irregularities in the expected timing and height of tides, further complicating our understanding of tidal patterns.Understanding the retardation of tide is essential for various sectors, including navigation, fishing, and coastal management. Mariners rely on accurate tidal information to ensure safe passage through coastal waters. Delays in tidal movements can impact shipping schedules and fishing operations, making it crucial for those involved in these industries to account for potential retardation effects.In addition to practical applications, studying the retardation of tide helps scientists understand broader environmental changes. As sea levels rise due to climate change, the dynamics of tidal movements may also shift. By monitoring these changes, researchers can gain insights into the health of coastal ecosystems and the potential impacts of human activity on natural tidal patterns.In conclusion, the retardation of tide is a complex phenomenon influenced by various factors, including geographical features, weather conditions, and human activities. Its implications extend beyond mere water level fluctuations, affecting ecosystems, economies, and our understanding of environmental changes. As we continue to study and monitor tidal behaviors, we can better prepare for the challenges posed by a changing climate and ensure the sustainability of our coastal regions.

潮汐的滞后现象是海洋学中一个迷人的方面，对沿海生态系统和人类活动具有重要影响。潮汐主要由月球和太阳的引力引起，表现出水位的周期性升降模式。然而，各种因素可以影响这种自然节奏，导致潮汐的滞后或潮汐运动的时间和高度延迟。造成潮汐滞后的主要原因之一是海洋与陆地之间的相互作用。当潮汐接近沿海地区时，它们与海床和海岸线产生摩擦。这种摩擦减缓了水的运动，导致潮汐的高峰与基于天文计算的预期时间相比出现延迟。这种现象在浅水区尤为明显，因为底部地形显著影响潮汐行为。另一个导致潮汐滞后的因素是大水体的存在，例如海湾和河口。这些区域可以困住水，导致水的升降速度与开放海洋不同。例如，当海湾中发生高潮时，由于水流进入狭窄空间受到限制，水可能需要更长的时间才能达到最高点。同样，在低潮期间，水的退去可能会更慢，从而导致潮汐模式的明显滞后。天气条件也在潮汐滞后中发挥着关键作用。风暴、风向和气压变化都可以影响潮汐运动。例如，强风可以将水推向海岸，导致水位暂时升高，而低气压则可以使水更容易上升。这些变化可能导致预期潮汐的时间和高度出现不规则性，进一步复杂化我们对潮汐模式的理解。理解潮汐的滞后对航行、捕鱼和沿海管理等各个领域至关重要。海员依赖准确的潮汐信息以确保安全通过沿海水域。潮汐运动的延迟可能会影响航运计划和捕鱼作业，因此从事这些行业的人必须考虑潜在的滞后效应。除了实际应用，研究潮汐的滞后还有助于科学家理解更广泛的环境变化。随着气候变化导致海平面上升，潮汐运动的动态也可能发生变化。通过监测这些变化，研究人员可以获得关于沿海生态系统健康状况和人类活动对自然潮汐模式潜在影响的见解。总之，潮汐的滞后是一个复杂的现象，受地理特征、天气条件和人类活动等多种因素的影响。它的影响超越了单纯的水位波动，影响生态系统、经济以及我们对环境变化的理解。随着我们继续研究和监测潮汐行为，我们可以更好地应对气候变化带来的挑战，并确保沿海地区的可持续发展。