thermocline

简明释义

英[ˈθɜːmə(ʊ)klaɪn]美[ˈθɜːrməˌklaɪn]

n. 变温层

英英释义

单词用法

同义词

反义词

例句

1.This paper introduces the major advances in the studies of the ventilated thermocline theory of ocean circulation.

介绍了大洋环流理论中通风温跃层研究的主要进展。

2.Thermocline is important for submarine in underwater navigation and action.

温跃层对于潜艇的水下航行和战斗具有十分重要的意义。

3.Interdecadal variability of the thermocline along the west coast of South America.

沿南美洲西海岸温跃层的十年间变化。

4.In summer, the temperature of the south part of the area is higher than the north part. Both the main thermocline and the main halocline are thin and their depths range from 50 to 120m.

第四章对历年温盐和表层流资料的进行了统计分析，给出了开辟区的温盐和表层流的分布特征和年变化特征：（1）表层水温在夏季呈南高北低的特点，温盐跃层较薄，中心位置在50～120米之间变化；

5.Both of these two types of forcings affect ENSO amplitude mainly by the adjustment of oceanic wave on the thermocline.

这些外强迫主要是通过海洋波动对斜温层深度的调节来影响ENSO事件的强度的。

6.Based on the theory of the local spectrum of ambient-sea noise field, theoretical models of the low-noise-channel for typical shallow-water negative gradient (or thermocline) are developed.

本文根据海洋噪声场随机局部谱展开理论，分析了典型浅海负梯度(或负跃层)下低噪声信道的理论模型。

7.The presence of a strong thermocline can impact the distribution of nutrients in the ocean.

强烈的温跃层的存在会影响海洋中营养物质的分布。

8.Scientists use buoys to monitor the thermocline and gather data for climate change studies.

科学家使用浮标监测温跃层，以收集气候变化研究的数据。

9.Divers often need to be aware of the thermocline as it can cause sudden temperature changes underwater.

潜水员常常需要注意温跃层，因为它可能导致水下温度的突然变化。

10.During the summer months, the thermocline can rise significantly, affecting the water temperature in lakes.

在夏季，温跃层可能会显著上升，影响湖泊的水温。

11.The research team measured the depth of the thermocline to study its effects on fish migration patterns.

研究小组测量了温跃层的深度，以研究其对鱼类迁徙模式的影响。

作文

The ocean is a vast and complex environment that plays a crucial role in regulating the Earth's climate. One of the key features of the ocean is the presence of different layers of water, each with its own temperature and density. Among these layers, the thermocline 温跃层 is particularly significant. The thermocline 温跃层 is a distinct layer in a body of water where the temperature changes rapidly with depth. This phenomenon occurs in both oceans and large lakes, and it serves as a barrier between the warmer, mixed surface waters and the colder, deeper waters.Understanding the thermocline 温跃层 is essential for various scientific fields, including oceanography, ecology, and climate science. The thermocline 温跃层 typically forms during the warmer months when sunlight heats the upper layers of water. As a result, the surface waters become significantly warmer than the layers below, creating a gradient of temperature that can affect marine life and ocean currents.One interesting aspect of the thermocline 温跃层 is its impact on marine ecosystems. Many fish and other marine organisms rely on the temperature gradients created by the thermocline 温跃层 for their survival. For instance, certain species of fish prefer the cooler waters just below the thermocline 温跃层, where they find abundant food sources and protection from predators. This makes the thermocline 温跃层 a vital area for fishing industries around the world.Moreover, the thermocline 温跃层 also influences the distribution of nutrients in the ocean. In many regions, the mixing of waters above and below the thermocline 温跃层 brings nutrients from the depths to the surface. This process is essential for phytoplankton growth, which forms the foundation of the marine food web. A healthy population of phytoplankton supports various marine species, from small fish to large whales.Climate change poses a significant threat to the stability of the thermocline 温跃层. As global temperatures rise, the warming of surface waters can lead to a more pronounced thermocline 温跃层, which can disrupt the natural mixing processes of the ocean. This disruption can result in decreased nutrient availability, affecting marine life and ecosystems. Additionally, changes in the thermocline 温跃层 can alter ocean currents, which play a critical role in regulating climate patterns worldwide.In conclusion, the thermocline 温跃层 is an essential feature of aquatic environments that has far-reaching implications for marine life, nutrient distribution, and climate regulation. Understanding this layer of water helps scientists predict the effects of climate change and manage marine resources effectively. As we continue to study the complexities of our oceans, the thermocline 温跃层 remains a focal point for research and conservation efforts, highlighting the interconnectedness of our planet's systems.

海洋是一个广阔而复杂的环境，在调节地球气候方面发挥着至关重要的作用。海洋的一个关键特征是存在不同的水层，每个水层都有其独特的温度和密度。在这些水层中，thermocline 温跃层尤其重要。thermocline 温跃层是在水体中一个明显的层次，在这个层次中，温度随着深度的变化而快速变化。这种现象发生在海洋和大型湖泊中，并且它作为温暖的混合表层水与较冷的深层水之间的屏障。理解thermocline 温跃层对于海洋学、生态学和气候科学等多个科学领域至关重要。thermocline 温跃层通常在温暖的月份形成，当阳光加热水的上层时。结果，表层水的温度显著高于下面的水层，从而造成温度梯度，这可以影响海洋生物和洋流。thermocline 温跃层的一个有趣方面是它对海洋生态系统的影响。许多鱼类和其他海洋生物依赖于thermocline 温跃层所创造的温度梯度来生存。例如，某些鱼类物种更喜欢位于thermocline 温跃层下方的较冷水域，在那里它们可以找到丰富的食物来源和保护免受捕食者的威胁。这使得thermocline 温跃层成为全球渔业的重要区域。此外，thermocline 温跃层还影响海洋中的营养物质分布。在许多地区，上下水层的混合过程将深层的营养物质带到表面。这个过程对浮游植物的生长至关重要，而浮游植物构成了海洋食物链的基础。健康的浮游植物种群支持各种海洋物种，从小鱼到大鲸鱼。气候变化对thermocline 温跃层的稳定性构成了重大威胁。随着全球气温上升，表层水的升温可能导致thermocline 温跃层变得更加明显，这可能会扰乱海洋的自然混合过程。这种干扰可能导致营养物质可用性的减少，影响海洋生物和生态系统。此外，thermocline 温跃层的变化可能改变洋流，而洋流在调节全球气候模式中发挥着关键作用。总之，thermocline 温跃层是水生环境中的一个重要特征，对海洋生物、营养分布和气候调节具有深远的影响。理解这一水层有助于科学家预测气候变化的影响并有效管理海洋资源。随着我们继续研究海洋的复杂性，thermocline 温跃层仍然是研究和保护工作的重点，突显了我们星球系统之间的相互联系。