tropic lower low water

简明释义

回归低低潮回归低低潮

英英释义

例句

1.Boaters should be aware of the Tropic Lower Low Water 热带最低潮水位 to avoid grounding their vessels.

船只操作者应注意Tropic Lower Low Water 热带最低潮水位，以避免搁浅。

2.When planning the construction of the pier, we had to consider the Tropic Lower Low Water 热带最低潮水位 to ensure stability.

在规划码头的建设时，我们必须考虑到Tropic Lower Low Water 热带最低潮水位以确保稳定性。

3.The marina is located just above the Tropic Lower Low Water 热带最低潮水位, making it a safe harbor during most conditions.

这个码头位于Tropic Lower Low Water 热带最低潮水位之上，因此在大多数情况下是一个安全的避风港。

4.The tidal charts indicate that the next Tropic Lower Low Water 热带最低潮水位 will occur at midnight.

潮汐图表显示下一个Tropic Lower Low Water 热带最低潮水位将在午夜发生。

5.Fishing activities are best scheduled around the Tropic Lower Low Water 热带最低潮水位 for optimal catch.

渔业活动最好安排在Tropic Lower Low Water 热带最低潮水位附近，以获得最佳捕捞效果。

作文

Understanding the concept of tropic lower low water is crucial for those involved in maritime activities, coastal management, and environmental studies. The term refers to a specific tidal measurement that is particularly relevant in tropical regions. Tides are the rise and fall of sea levels caused by the gravitational forces exerted by the moon and the sun, as well as the rotation of the Earth. In tropical areas, the tidal patterns can be quite distinct due to various geographical and climatic factors. tropic lower low water is defined as the lowest level of water that can be observed during the lowest tides, which typically occur during spring tides when the sun and moon are aligned. This measurement is significant for several reasons. For one, it provides essential data for navigation. Ships and boats must be aware of the tropic lower low water levels to avoid grounding on submerged obstacles or sandbars. Accurate tidal information helps mariners plan their routes and schedules effectively, ensuring safe passage through shallow waters. Furthermore, knowledge of these water levels is vital for coastal construction projects. Engineers and architects need to consider the tropic lower low water when designing docks, piers, and other structures that interact with the ocean. Failure to account for these levels could result in costly mistakes, such as building too close to the shoreline or underestimating the impact of erosion.In addition to its practical applications, understanding tropic lower low water also has ecological implications. Coastal ecosystems, such as mangroves and coral reefs, are sensitive to changes in tidal patterns. By monitoring the tropic lower low water, researchers can assess the health of these environments and identify potential threats from climate change, pollution, and human activity. For example, if sea levels rise due to global warming, the tropic lower low water mark may shift, affecting the habitats of various marine species and altering the dynamics of the ecosystem.Moreover, the tropic lower low water serves as a reference point for measuring sea level rise. Scientists use this data to understand how climate change is impacting coastal regions. By comparing historical tropic lower low water measurements with current data, researchers can gauge the rate of sea-level rise and its potential consequences for coastal communities. This information is vital for policymakers who need to make informed decisions about land use, disaster preparedness, and environmental protection.In conclusion, the concept of tropic lower low water is essential for navigation, coastal engineering, ecological studies, and climate research. Its significance extends beyond mere measurement; it plays a critical role in ensuring safety at sea, protecting coastal infrastructures, and preserving delicate marine ecosystems. As our understanding of tidal patterns and their impacts continues to grow, so too does the importance of accurately measuring and interpreting the tropic lower low water. Those engaged in maritime activities, environmental science, and coastal management must prioritize this knowledge to promote sustainable practices and safeguard our oceans for future generations.

理解热带低潮水位这个概念对于参与海事活动、沿海管理和环境研究的人来说至关重要。这个术语指的是一个特定的潮汐测量，尤其与热带地区相关。潮汐是由月球和太阳施加的引力以及地球的自转引起的海平面升降。在热带地区，由于各种地理和气候因素，潮汐模式可能相当独特。热带低潮水位被定义为在最低潮期间观察到的最低水位，这通常发生在春潮期间，即太阳和月亮处于对齐状态时。这个测量具有几个重要原因。首先，它为航行提供了必要的数据。船只和小艇必须了解热带低潮水位水平，以避免在淹没的障碍物或沙洲上搁浅。准确的潮汐信息帮助航海者有效地规划航线和时间表，确保安全通过浅水区。此外，了解这些水位对于沿海建设项目至关重要。工程师和建筑师在设计码头、栈桥和其他与海洋互动的结构时，需要考虑热带低潮水位。未能考虑这些水平可能导致代价高昂的错误，例如建造得离海岸线太近或低估侵蚀的影响。除了实际应用外，理解热带低潮水位还有生态意义。沿海生态系统，如红树林和珊瑚礁，对潮汐模式的变化非常敏感。通过监测热带低潮水位，研究人员可以评估这些环境的健康状况，并识别气候变化、污染和人类活动带来的潜在威胁。例如，如果由于全球变暖而海平面上升，热带低潮水位标志可能会移动，影响各种海洋物种的栖息地并改变生态系统的动态。此外，热带低潮水位作为测量海平面上升的参考点。科学家利用这些数据来了解气候变化如何影响沿海地区。通过将历史的热带低潮水位测量与当前数据进行比较，研究人员可以衡量海平面上升的速度及其对沿海社区的潜在影响。这些信息对政策制定者至关重要，他们需要就土地使用、灾害准备和环境保护做出明智的决策。总之，热带低潮水位的概念对于航行、沿海工程、生态研究和气候研究至关重要。它的重要性超越了单纯的测量；它在确保海上安全、保护沿海基础设施和维护脆弱的海洋生态系统方面发挥着关键作用。随着我们对潮汐模式及其影响的理解不断加深，准确测量和解释热带低潮水位的重要性也随之增加。参与海事活动、环境科学和沿海管理的人必须优先考虑这一知识，以促进可持续实践并保护我们的海洋，以造福未来世代。