cyclogenesis

简明释义

英[ˌsaɪkləʊˈdʒenɪsɪs]美[ˌsaɪkləˈdʒenəsɪs]

n. 风暴之发展形成

英英释义

单词用法

同义词

反义词

例句

1.We primarily discuss orographic effect on the synoptic system, and study the problems of lee cyclogenesis in the baroclinic atmosphere.

本文主要讨论地形对天气系统的影响，研究了斜压大气中地形背风气旋的问题。

2.We primarily discuss orographic effect on the synoptic system, and study the problems of lee cyclogenesis in the baroclinic atmosphere.

本文主要讨论地形对天气系统的影响，研究了斜压大气中地形背风气旋的问题。

3.Understanding cyclogenesis helps in forecasting hurricanes and tropical storms.

理解气旋生成有助于预测飓风和热带风暴。

4.Meteorologists study the process of cyclogenesis to predict severe weather patterns.

气象学家研究气旋生成的过程以预测严重的天气模式。

5.The cyclogenesis that occurred last night resulted in heavy rainfall across the region.

昨晚发生的气旋生成导致该地区出现了大雨。

6.The rapid cyclogenesis off the coast surprised many meteorologists.

沿海迅速的气旋生成让许多气象学家感到惊讶。

7.Research on cyclogenesis is crucial for improving climate models.

对气旋生成的研究对改善气候模型至关重要。

作文

The phenomenon of weather patterns is a complex and fascinating subject, particularly when we delve into the processes that lead to the formation of storms. One such process is known as cyclogenesis, which refers to the development and intensification of a low-pressure system in the atmosphere. Understanding cyclogenesis is crucial for meteorologists as it helps them predict severe weather events such as hurricanes, tornadoes, and winter storms. To grasp the concept of cyclogenesis, we must first understand the conditions that contribute to its occurrence. Typically, cyclogenesis takes place in regions where there are significant temperature differences, such as along fronts where warm and cold air masses meet. The interaction between these air masses can create instability in the atmosphere, leading to the formation of a cyclone. This process can be influenced by various factors, including topography, sea surface temperatures, and prevailing winds.There are two main types of cyclogenesis: tropical and extratropical. Tropical cyclogenesis occurs over warm ocean waters and is characterized by the formation of tropical storms and hurricanes. These systems are fueled by the heat and moisture from the ocean, which causes the air to rise and create a low-pressure area. As the storm develops, it can grow in intensity, leading to potentially devastating impacts on coastal communities.On the other hand, extratropical cyclogenesis typically occurs in mid-latitude regions and is associated with frontal systems. In this case, the collision of warm and cold air masses can lead to the formation of a low-pressure system that can bring about severe weather, including heavy rain, snow, and strong winds. Extratropical cyclones often travel across the continent, affecting large areas and causing significant weather changes.The study of cyclogenesis is not only important for understanding weather patterns but also for preparing for natural disasters. Meteorologists utilize advanced technology and models to track the development of low-pressure systems and predict their paths. By analyzing data related to cyclogenesis, they can issue warnings to communities at risk, allowing people to take necessary precautions.In conclusion, cyclogenesis plays a vital role in the Earth's weather systems. It is the process through which low-pressure systems form and intensify, leading to various weather phenomena. By studying cyclogenesis, scientists can better understand and predict severe weather events, ultimately helping to protect lives and property. As climate change continues to impact our planet, the importance of understanding cyclogenesis and its implications for weather patterns will only grow, making it a critical area of research for the future.

天气模式的现象是一个复杂而迷人的主题，特别是当我们深入探讨导致风暴形成的过程时。其中一个过程被称为气旋生成，指的是大气中低压系统的发展和增强。理解气旋生成对气象学家至关重要，因为它帮助他们预测严重的天气事件，如飓风、龙卷风和冬季风暴。要掌握气旋生成的概念，我们首先必须了解促成其发生的条件。通常，气旋生成发生在温度差异显著的地区，例如温暖和寒冷气团相遇的锋面。气团之间的相互作用可以在大气中产生不稳定性，导致气旋的形成。这个过程可能受到多种因素的影响，包括地形、海面温度和盛行风。气旋生成主要有两种类型：热带和外热带。热带气旋生成发生在温暖的海洋水域，特征是热带风暴和飓风的形成。这些系统由海洋的热量和湿气提供动力，导致空气上升并形成低压区。随着风暴的发展，它可能会增强强度，对沿海社区造成潜在的破坏性影响。另一方面，外热带气旋生成通常发生在中纬度地区，与锋面系统相关。在这种情况下，温暖和寒冷气团的碰撞可以导致低压系统的形成，可能带来严重的天气，包括大雨、降雪和强风。外热带气旋通常穿越大陆，影响大面积区域并导致显著的天气变化。对气旋生成的研究不仅对理解天气模式重要，而且对自然灾害的准备也很重要。气象学家利用先进的技术和模型来跟踪低压系统的发展并预测其路径。通过分析与气旋生成相关的数据，他们可以向面临风险的社区发布警报，使人们能够采取必要的预防措施。总之，气旋生成在地球的天气系统中发挥着至关重要的作用。它是低压系统形成和增强的过程，导致各种天气现象。通过研究气旋生成，科学家可以更好地理解和预测严重的天气事件，最终帮助保护生命和财产。随着气候变化继续影响我们的星球，理解气旋生成及其对天气模式的影响的重要性只会增加，这使其成为未来关键的研究领域。