mean diurnal high water inequality

简明释义

平均日潮高潮不等日潮高潮不等平均日高潮不等

英英释义

例句

1.The coastal engineers calculated the mean diurnal high water inequality to predict tidal patterns for the new marina project.

沿海工程师计算了平均昼夜高潮不等式以预测新码头项目的潮汐模式。

2.When designing seawalls, engineers must account for the mean diurnal high water inequality to ensure effectiveness.

在设计海堤时，工程师必须考虑平均昼夜高潮不等式以确保有效性。

3.Local authorities used the mean diurnal high water inequality data to improve flood management strategies.

地方当局利用平均昼夜高潮不等式数据来改善洪水管理策略。

4.The research team published a paper on the effects of mean diurnal high water inequality on coastal erosion.

研究小组发表了一篇关于平均昼夜高潮不等式对海岸侵蚀影响的论文。

5.Understanding the mean diurnal high water inequality is crucial for fishermen planning their trips around the tides.

了解平均昼夜高潮不等式对于计划潮汐出行的渔民至关重要。

作文

Understanding the concept of mean diurnal high water inequality is essential for those involved in marine science, coastal engineering, and environmental studies. This term refers to the average difference in height between the highest tides that occur over a 24-hour period. Tides are primarily influenced by the gravitational pull of the moon and the sun, as well as the rotation of the Earth. The mean diurnal high water inequality can vary significantly depending on geographical location, lunar phases, and local topography.In regions where the tidal range is predominantly semi-diurnal, such as the Atlantic coast of the United States, the mean diurnal high water inequality tends to be less pronounced. Here, there are typically two high tides and two low tides each day, leading to a more even distribution of tidal heights. However, in areas with a diurnal tide regime, like certain parts of the Gulf of Mexico and the Caribbean, the mean diurnal high water inequality can be quite significant, resulting in one high tide being considerably higher than the other.The implications of understanding mean diurnal high water inequality extend beyond academic interest; they have practical applications in navigation, fishing, and coastal management. For instance, fishermen often rely on tidal patterns to determine the best times to catch certain species. Knowing when the tides will be at their highest can help them optimize their efforts, as some fish are more active during these periods. Additionally, coastal engineers must consider mean diurnal high water inequality when designing structures such as docks, seawalls, and marinas. If they underestimate the potential height of high tides, it could lead to costly damages and safety hazards.Moreover, climate change poses a challenge to our understanding of mean diurnal high water inequality. As sea levels rise, the dynamics of tides may also shift, potentially altering the patterns of high and low water marks. This can have significant consequences for coastal ecosystems, which rely on specific tidal conditions to thrive. Changes in tidal patterns can affect sediment transport, erosion rates, and habitat availability for various marine species.In conclusion, the mean diurnal high water inequality is a vital concept for anyone studying or working in fields related to oceanography and coastal science. Its understanding not only aids in scientific research but also has real-world applications that impact various industries and ecosystems. By recognizing the importance of this term, we can better appreciate the complexities of tidal systems and their influence on our environment. As we continue to face challenges related to climate change, a deeper understanding of tidal dynamics, including mean diurnal high water inequality, will be crucial in developing strategies for sustainable coastal management and conservation efforts.

理解平均日间高水不等式的概念对于那些从事海洋科学、海岸工程和环境研究的人来说至关重要。这个术语指的是在24小时内发生的最高潮位之间的平均高度差。潮汐主要受月球和太阳的引力以及地球的自转影响。平均日间高水不等式可以根据地理位置、月相和当地地形的不同而显著变化。在潮汐范围主要为半日潮的地区，例如美国大西洋沿岸，平均日间高水不等式往往不那么明显。在这里，通常每天会有两个高潮和两个低潮，从而导致潮位高度的更均匀分布。然而，在某些墨西哥湾和加勒比地区的潮汐制度为日潮的区域，平均日间高水不等式可能相当显著，导致一个高潮的高度远高于另一个。理解平均日间高水不等式的意义超越了学术兴趣；它在航行、捕鱼和海岸管理等方面有实际应用。例如，渔民常常依赖潮汐模式来确定捕捞某些物种的最佳时机。了解潮水何时达到最高可以帮助他们优化捕捞工作，因为某些鱼类在这些时期更为活跃。此外，海岸工程师在设计码头、海堤和码头时必须考虑平均日间高水不等式。如果他们低估了高潮的潜在高度，可能会导致昂贵的损失和安全隐患。此外，气候变化对我们理解平均日间高水不等式构成了挑战。随着海平面上升，潮汐的动态也可能发生变化，可能改变高低水位的模式。这对依赖特定潮汐条件生存的沿海生态系统产生重大影响。潮汐模式的变化可能会影响沉积物运输、侵蚀率以及各种海洋物种的栖息地可用性。总之，平均日间高水不等式是任何研究或从事与海洋学和海岸科学相关领域的人必备的重要概念。它的理解不仅有助于科学研究，还有现实世界的应用，影响着各个行业和生态系统。通过认识到这个术语的重要性，我们可以更好地欣赏潮汐系统的复杂性及其对我们环境的影响。随着我们继续面临与气候变化相关的挑战，更深入地理解潮汐动态，包括平均日间高水不等式，在制定可持续的海岸管理和保护措施方面至关重要。