retardation of tide

简明释义

潮汐延迟潮汐迟滞差

英英释义

The delay or slowing down of the movement of tidal waters, often caused by factors such as geographical features, weather conditions, or human activities.

潮水运动的延迟或减缓,通常由地理特征、天气条件或人类活动等因素引起。

例句

1.Understanding the retardation of tide is crucial for predicting coastal erosion patterns.

理解潮汐延迟对预测海岸侵蚀模式至关重要。

2.The retardation of tide can affect navigation routes for shipping vessels.

潮汐的延迟可能影响船舶的航行路线。

3.The engineer studied the retardation of tide in the bay to improve the design of the new harbor.

工程师研究了海湾的潮汐延迟以改善新港口的设计。

4.The research focused on the retardation of tide during storm surges.

研究集中在风暴潮期间的潮汐延迟

5.Scientists measured the retardation of tide to understand its impact on marine life.

科学家测量了潮汐延迟以了解其对海洋生物的影响。

作文

The phenomenon of the retardation of tide can be observed in various coastal regions around the world. Tides are primarily caused by the gravitational pull of the moon and the sun on Earth's oceans, creating a regular rise and fall of sea levels. However, this natural rhythm can be disrupted by several factors, leading to what is known as the retardation of tide (潮汐延迟). Understanding this concept is crucial for marine navigation, coastal management, and environmental studies.One of the primary causes of the retardation of tide is the geography of the coastline. In areas where the seabed is shallow or where there are numerous islands, the flow of water can be impeded, causing delays in the tidal movement. For example, in a bay with a narrow entrance, the incoming tide may take longer to fill the area behind the entrance compared to an open ocean. This geographical influence means that different locations experience tides at different times, leading to variations in tidal patterns.Another significant factor contributing to the retardation of tide is the meteorological conditions. Weather events such as storms, wind patterns, and atmospheric pressure can drastically alter tidal behavior. During a storm, strong winds can push water towards the shore, leading to higher than normal tide levels, while low atmospheric pressure can cause the water level to drop. These changes can cause a lag in the expected timing of high and low tides, illustrating how external forces can impact the natural tidal cycle.Moreover, human activities also play a role in the retardation of tide. Coastal development, such as the construction of ports, jetties, and seawalls, can disrupt the natural flow of water. These structures can create barriers that prevent water from moving freely, resulting in delayed tidal movements. Additionally, dredging activities can alter the seabed, further impacting the timing and height of tides in affected areas. As coastal populations continue to grow, it becomes increasingly important to consider the implications of these developments on tidal behavior.The retardation of tide is not just a scientific curiosity; it has practical implications for various industries. For fishermen, understanding the timing of tides is essential for planning fishing trips. Similarly, for ship captains, knowledge of tidal patterns can be the difference between a safe voyage and a navigational disaster. Furthermore, coastal engineers must account for tidal delays when designing infrastructure to ensure safety and functionality.In conclusion, the retardation of tide is a multifaceted phenomenon influenced by geographic, meteorological, and anthropogenic factors. As we continue to study and understand these influences, we can better prepare for their effects on our coastal environments. Whether for scientific research, maritime navigation, or environmental conservation, a thorough grasp of the retardation of tide is essential for anyone involved in coastal activities. By acknowledging and adapting to these tidal variations, we can work towards sustainable management of our precious marine resources.

潮汐延迟现象可以在世界各地的不同沿海地区观察到。潮汐主要是由月球和太阳对地球海洋的引力引起的,造成海平面的定期升降。然而,这种自然节奏可能会被多种因素打断,导致所谓的潮汐延迟(retardation of tide)。理解这一概念对于海洋导航、沿海管理和环境研究至关重要。潮汐延迟的主要原因之一是海岸线的地理特征。在海床较浅或有众多岛屿的地区,水流可能受到阻碍,从而导致潮汐运动的延迟。例如,在一个入口狭窄的海湾,进入的潮水可能需要更长时间才能填满入口后的区域,而与开放海洋相比。这种地理影响意味着不同地点的潮汐在不同时间发生,导致潮汐模式的变化。另一个显著影响潮汐延迟的因素是气象条件。天气事件如风暴、风向和气压变化能够大幅改变潮汐行为。在风暴期间,强风可以将水推向海岸,导致潮位高于正常水平,而低气压则可能导致水位下降。这些变化可能导致预期的高潮和低潮的时间出现滞后,说明外部力量如何影响自然潮汐周期。此外,人类活动也在潮汐延迟中发挥着作用。沿海开发,如港口、码头和防波堤的建设,可能会干扰自然水流。这些结构可能形成障碍,阻止水自由流动,从而导致潮汐运动的延迟。此外,疏浚活动可能改变海床,进一步影响受影响区域的潮汐时间和高度。随着沿海人口的不断增长,考虑这些开发对潮汐行为影响的重要性愈发突出。潮汐延迟不仅是一个科学好奇心,它对各个行业都有实际影响。对于渔民来说,了解潮汐的时机对于计划捕鱼活动至关重要。同样,对于船长而言,了解潮汐模式可以决定安全航行与否。此外,沿海工程师在设计基础设施时必须考虑潮汐延迟,以确保安全和功能性。总之,潮汐延迟是一个多方面的现象,受地理、气象和人为因素的影响。随着我们继续研究和理解这些影响,我们可以更好地为其对沿海环境的影响做好准备。无论是出于科学研究、海洋导航还是环境保护,全面掌握潮汐延迟对参与沿海活动的任何人来说都是至关重要的。通过承认和适应这些潮汐变化,我们可以朝着可持续管理我们珍贵的海洋资源努力。

相关单词

retardation

retardation详解:怎么读、什么意思、用法

tide

tide详解:怎么读、什么意思、用法