mean diurnal high water inequality

简明释义

平均日潮高潮不等

英英释义

Mean diurnal high water inequality refers to the average difference in height between the highest high tide and the lowest high tide that occurs within a 24-hour period.

平均昼夜高潮不平衡是指在24小时内,最高潮位和最低潮位之间的平均高度差。

例句

1.The mean diurnal high water inequality affects navigation routes for ships in the harbor.

对于港口的船只航线,平均日间高潮水位不平等影响显著。

2.The study analyzed the mean diurnal high water inequality to understand tidal patterns better.

该研究分析了平均日间高潮水位不平等以更好地理解潮汐模式。

3.Researchers measured the mean diurnal high water inequality to predict flooding events.

研究人员测量了平均日间高潮水位不平等以预测洪水事件。

4.Understanding the mean diurnal high water inequality is crucial for fisheries management.

理解平均日间高潮水位不平等对渔业管理至关重要。

5.Engineers need to consider the mean diurnal high water inequality when designing coastal structures.

工程师在设计沿海结构时需要考虑平均日间高潮水位不平等

作文

Understanding the concept of mean diurnal high water inequality is crucial for anyone studying tidal patterns and their effects on coastal environments. Tides are a natural phenomenon caused by the gravitational pull of the moon and the sun on Earth's waters. The variation in water levels, particularly during high tide, can significantly impact marine ecosystems, navigation, and coastal development. Mean diurnal high water inequality, specifically, refers to the difference in height between the highest high tide and the lowest high tide within a single day. This concept is important because it helps researchers and environmentalists predict tidal behaviors and understand how they influence various factors such as sediment transport, salinity levels, and habitat availability for marine species.In coastal areas, the mean diurnal high water inequality can vary greatly due to several factors including geographical location, local wind patterns, and atmospheric pressure. For instance, some regions may experience mixed tides where both semi-diurnal (two high tides and two low tides each day) and diurnal (one high tide and one low tide each day) patterns occur, leading to greater inequality in water heights. Understanding this inequality helps in planning for coastal infrastructure projects, as engineers must consider how varying water levels could affect their designs.Moreover, the mean diurnal high water inequality also plays a significant role in the behavior of marine organisms. Many species have adapted to the rhythms of tidal changes. For example, certain fish and crustaceans time their spawning to coincide with high tides, ensuring that their offspring are carried into safer, deeper waters. If the high water levels are inconsistent due to a large mean diurnal high water inequality, it can disrupt these natural cycles, potentially impacting population dynamics.Additionally, climate change poses a threat to the traditional patterns of tides and the associated mean diurnal high water inequality. Rising sea levels and increased storm frequency can lead to more pronounced tidal fluctuations, which may alter existing ecosystems and create challenges for coastal communities. As such, understanding the implications of this inequality becomes increasingly important in the face of environmental changes. In conclusion, the study of mean diurnal high water inequality is essential for managing coastal environments and protecting marine life. By analyzing tidal patterns and their variations, scientists can better predict ecological outcomes and inform policy decisions regarding coastal management. As we continue to grapple with the impacts of climate change, a thorough understanding of tidal dynamics will be vital in preserving our oceans and the diverse life they support. Therefore, recognizing and studying mean diurnal high water inequality is not just an academic exercise; it is a necessary endeavor for the health of our planet's marine ecosystems and the communities that rely on them.

理解“平均昼夜高潮水位不平衡”这一概念对于任何研究潮汐模式及其对沿海环境影响的人来说都是至关重要的。潮汐是由月球和太阳对地球水体的引力作用引起的自然现象。水位的变化,尤其是在高潮期间,可能会显著影响海洋生态系统、航行和沿海开发。“平均昼夜高潮水位不平衡”特别指的是在一天内最高高潮与最低高潮之间的高度差。这一概念的重要性在于,它帮助研究人员和环保主义者预测潮汐行为,并理解它们如何影响诸如沉积物运输、盐度水平和海洋物种栖息地可用性等各种因素。在沿海地区,“平均昼夜高潮水位不平衡”可能因多种因素而大相径庭,包括地理位置、当地风向和气压。例如,一些地区可能会经历混合潮,即同时出现半日潮(每天两次高潮和两次低潮)和昼潮(每天一次高潮和一次低潮),从而导致水位高度的不平衡加剧。理解这种不平衡有助于规划沿海基础设施项目,因为工程师必须考虑到变化的水位如何影响他们的设计。此外,“平均昼夜高潮水位不平衡”在海洋生物的行为中也发挥着重要作用。许多物种已经适应了潮汐变化的节奏。例如,某些鱼类和甲壳类动物会将产卵时间与高潮相吻合,以确保后代被带入更安全、更深的水域。如果由于较大的“平均昼夜高潮水位不平衡”导致高潮水位不一致,这可能会扰乱这些自然周期,从而潜在地影响种群动态。此外,气候变化对潮汐的传统模式和相关的“平均昼夜高潮水位不平衡”构成威胁。海平面上升和风暴频率增加可能导致潮汐波动更加明显,这可能改变现有生态系统并给沿海社区带来挑战。因此,在面对环境变化时,理解这种不平衡的影响变得越来越重要。总之,研究“平均昼夜高潮水位不平衡”对于管理沿海环境和保护海洋生物至关重要。通过分析潮汐模式及其变化,科学家可以更好地预测生态结果并为沿海管理提供政策决策依据。随着我们继续应对气候变化的影响,深入理解潮汐动态将对保护我们的海洋及其支持的多样生命至关重要。因此,认识和研究“平均昼夜高潮水位不平衡”不仅仅是学术研究,而是为了我们星球海洋生态系统和依赖它们的社区的健康而进行的必要努力。

相关单词

diurnal

diurnal详解:怎么读、什么意思、用法

inequality

inequality详解:怎么读、什么意思、用法