continental anti-cyclone

简明释义

大陆反气旋

英英释义

例句

1.Meteorologists often track the movement of a continental anti-cyclone 大陆反气旋 to predict heatwaves in the summer.

气象学家经常追踪大陆反气旋 continental anti-cyclone的移动，以预测夏季的热浪。

2.A continental anti-cyclone 大陆反气旋 can create stable atmospheric conditions that suppress cloud formation.

一个大陆反气旋 continental anti-cyclone可以创造稳定的大气条件，抑制云的形成。

3.The presence of a continental anti-cyclone 大陆反气旋 typically results in clear skies and high temperatures.

一个大陆反气旋 continental anti-cyclone的存在通常会导致晴朗的天空和高温。

4.During winter, a strong continental anti-cyclone 大陆反气旋 can lead to prolonged periods of cold and dry weather.

在冬季，强烈的大陆反气旋 continental anti-cyclone可能导致长时间的寒冷和干燥天气。

5.Farmers monitor continental anti-cyclones 大陆反气旋 because they can significantly affect crop yields due to dry conditions.

农民监测大陆反气旋 continental anti-cyclones，因为它们可能因干燥条件而显著影响作物产量。

作文

A continental anti-cyclone is a significant meteorological phenomenon that occurs when high-pressure systems dominate the atmosphere over large land masses. These systems are characterized by descending air, which leads to clear skies and stable weather conditions. Understanding the dynamics of a continental anti-cyclone is crucial for meteorologists and anyone interested in weather patterns, as it can have profound effects on local climates and ecosystems.The formation of a continental anti-cyclone typically occurs during the winter months when the land cools more rapidly than the surrounding oceans. This temperature differential creates a high-pressure area over the land, where the air is denser and sinks. As the air descends, it warms up and dries out, leading to the formation of clear and calm weather. In contrast, regions under low-pressure systems often experience cloud formation and precipitation due to rising air.One of the most notable impacts of a continental anti-cyclone is its ability to influence regional climates. For instance, during the winter, a strong continental anti-cyclone can lead to prolonged periods of cold and dry weather in certain areas, while other regions may experience milder temperatures. This phenomenon can also contribute to drought conditions in places that rely on regular rainfall, as the stable weather prevents the development of storm systems that would typically bring precipitation.In addition to affecting temperature and precipitation patterns, a continental anti-cyclone can also play a role in air quality. The stable atmospheric conditions associated with high-pressure systems can trap pollutants close to the ground, leading to poor air quality in urban areas. This can pose health risks for residents, particularly those with respiratory conditions, and necessitates careful monitoring by environmental agencies.Furthermore, the presence of a continental anti-cyclone can influence weather events far beyond its immediate location. For example, it can steer storm systems away from certain regions, creating a protective barrier against severe weather. Conversely, the absence of a continental anti-cyclone might allow storms to develop and move into areas that are otherwise shielded, leading to unexpected weather changes.In conclusion, a continental anti-cyclone is a fundamental aspect of our planet's weather systems. Its ability to create stable, clear weather and influence regional climates makes it an important subject of study within meteorology. By understanding how these high-pressure systems form and behave, we can better prepare for the various weather conditions they bring. This knowledge is not only essential for forecasting but also for mitigating the potential impacts on agriculture, water resources, and public health. As climate change continues to alter weather patterns globally, the study of continental anti-cyclones and their effects will become increasingly vital for understanding our changing environment.

大陆反气旋是一个重要的气象现象，当高压系统在大面积陆地上占主导地位时就会发生。这些系统的特点是空气下沉，这导致晴朗的天空和稳定的天气条件。理解大陆反气旋的动态对于气象学家和任何对天气模式感兴趣的人来说都是至关重要的，因为它可以对当地气候和生态系统产生深远的影响。大陆反气旋的形成通常发生在冬季，当陆地比周围海洋冷却得更快时。这种温差在陆地上形成了一个高压区，空气更密集并下沉。随着空气下沉，它变暖并干燥，从而导致晴朗和宁静的天气形成。相比之下，处于低压系统下的区域往往由于空气上升而经历云层形成和降水。大陆反气旋最显著的影响之一是其能够影响区域气候。例如，在冬季，强烈的大陆反气旋可能导致某些地区长时间出现寒冷和干燥的天气，而其他地区可能经历较温和的气温。这种现象还可能导致依赖定期降雨的地方出现干旱条件，因为稳定的天气阻止了通常会带来降水的风暴系统的发展。除了影响温度和降水模式外，大陆反气旋还可以在空气质量方面发挥作用。与高压系统相关的稳定大气条件可能会将污染物困在靠近地面的地方，从而导致城市地区的空气质量下降。这可能对居民构成健康风险，特别是那些有呼吸道疾病的人，因此需要环境机构进行仔细监测。此外，大陆反气旋的存在还可以影响远离其直接位置的天气事件。例如，它可以将风暴系统引导远离某些地区，形成对严重天气的保护屏障。相反，大陆反气旋的缺失可能允许风暴发展并移动到通常受到保护的地区，导致意想不到的天气变化。总之，大陆反气旋是我们星球天气系统的基本方面。它创造稳定、晴朗天气的能力以及影响区域气候的能力使其成为气象学研究的重要主题。通过了解这些高压系统如何形成和运作，我们可以更好地为它们带来的各种天气条件做好准备。这一知识不仅对天气预报至关重要，还对减轻对农业、水资源和公共健康的潜在影响至关重要。随着气候变化继续改变全球天气模式，对大陆反气旋及其影响的研究将变得越来越重要，以理解我们不断变化的环境。