strength of ebb interval

简明释义

落潮流间隙

英英释义

例句

1.During low tide, the strength of ebb interval can reveal hidden rocks and hazards.

在低潮期间，退潮强度可以揭示隐藏的岩石和危险。

2.The fisherman adjusted his nets according to the strength of ebb interval to maximize his catch.

渔夫根据退潮强度调整渔网，以最大化捕获量。

3.Understanding the strength of ebb interval is crucial for sailing safely in coastal waters.

了解退潮强度对于在沿海水域安全航行至关重要。

4.Kayakers need to be aware of the strength of ebb interval to avoid strong currents.

皮划艇运动员需要注意退潮强度以避免强流。

5.The marine biologist studied how the strength of ebb interval affects local fish populations.

海洋生物学家研究了退潮强度如何影响当地鱼类种群。

作文

The concept of the strength of ebb interval is often overlooked in discussions about tides and their impact on coastal environments. Ebb intervals refer to the period during which the tide is receding, and understanding the strength of this phase is crucial for various ecological and geological processes. The strength of ebb interval can significantly influence sediment transport, nutrient cycling, and the overall health of marine ecosystems. To begin with, the strength of ebb interval plays a vital role in sediment transport. As the tide goes out, water carries with it sediments from the shore and the seabed. The stronger the ebb, the more sediment is removed from these areas. This process can lead to the formation of new landforms and the alteration of existing ones. For instance, strong ebb currents can create channels and grooves in the seabed, which can affect local habitats and the organisms that live there. Moreover, the strength of ebb interval also impacts nutrient cycling. During ebb tides, nutrients that have accumulated in tidal pools and estuaries are released back into the ocean. A stronger ebb can enhance this process, allowing for a more significant exchange of nutrients between coastal and open ocean waters. This nutrient influx is vital for supporting marine life, particularly in areas where nutrient levels may otherwise be low. Consequently, the strength of ebb interval is not only a physical phenomenon but also a biological one, influencing the productivity of marine ecosystems. In addition to its ecological significance, the strength of ebb interval has implications for human activities as well. Coastal communities often rely on fishing and tourism, both of which can be affected by tidal patterns. Understanding the strength of ebb interval can help fishermen determine the best times to catch certain species, as many fish are more active during specific tidal phases. Similarly, tourists who visit coastal areas may prefer to engage in activities such as beachcombing or kayaking during low tide when the effects of the ebb are most pronounced. Furthermore, the strength of ebb interval can influence coastal erosion and habitat loss. In areas where the ebb is particularly strong, the shoreline may experience accelerated erosion, leading to the loss of valuable land and habitats. This can have detrimental effects on local wildlife and can also threaten human infrastructure. Understanding how to measure and predict the strength of ebb interval is essential for developing effective coastal management strategies aimed at mitigating these impacts. In conclusion, the strength of ebb interval is a critical factor in understanding the dynamics of coastal environments. Its influence extends beyond mere physical changes in the landscape; it affects sediment transport, nutrient cycling, and the health of marine ecosystems. Additionally, it has practical implications for human activities such as fishing and tourism. As we continue to study and monitor our oceans, recognizing the importance of the strength of ebb interval will be essential for promoting sustainable practices and protecting our coastal resources.

“退潮间隔的强度”这一概念在讨论潮汐及其对沿海环境影响时常常被忽视。退潮间隔是指潮水退去的阶段，理解这一阶段的强度对于各种生态和地质过程至关重要。“退潮间隔的强度”可以显著影响沉积物运输、营养物质循环以及海洋生态系统的整体健康。首先，“退潮间隔的强度”在沉积物运输中起着重要作用。当潮水退去时，水流带走岸边和海底的沉积物。退潮越强，从这些区域移走的沉积物就越多。这一过程可能导致新地形的形成以及现有地形的改变。例如，强烈的退潮流可以在海底形成水道和沟槽，这可能会影响当地栖息地及其生物。此外，“退潮间隔的强度”还影响营养物质循环。在退潮时，积累在潮池和河口的营养物质被释放回海洋。更强的退潮可以增强这一过程，促进沿海与开放海域之间营养物质的更大交换。这种营养物质的流入对支持海洋生物至关重要，特别是在那些营养水平可能较低的区域。因此，“退潮间隔的强度”不仅是一个物理现象，也是一个生物现象，影响着海洋生态系统的生产力。除了生态意义外，“退潮间隔的强度”也对人类活动产生影响。沿海社区通常依赖于捕鱼和旅游，而这些活动都可能受到潮汐模式的影响。理解“退潮间隔的强度”可以帮助渔民确定捕捞某些物种的最佳时机，因为许多鱼在特定的潮汐阶段更为活跃。同样，前往沿海地区的游客可能更喜欢在低潮期间进行如海滩漫步或皮划艇等活动，此时退潮的效果最为明显。此外，“退潮间隔的强度”还可能影响沿海侵蚀和栖息地丧失。在退潮特别强的区域，海岸线可能会经历加速侵蚀，导致宝贵土地和栖息地的丧失。这可能对当地野生动物造成不利影响，也可能威胁到人类基础设施。理解如何测量和预测“退潮间隔的强度”对于制定有效的沿海管理策略以减轻这些影响至关重要。总之，“退潮间隔的强度”是在理解沿海环境动态时的一个关键因素。它的影响不仅限于景观的物理变化；它还影响沉积物运输、营养物质循环以及海洋生态系统的健康。此外，它对捕鱼和旅游等人类活动也具有实际意义。随着我们继续研究和监测海洋，认识到“退潮间隔的强度”的重要性将对促进可持续实践和保护沿海资源至关重要。