cold occlusion front

简明释义

冷锢囚锋

英英释义

A cold occlusion front is a type of weather front that occurs when a colder air mass overtakes a warmer air mass, causing the warm air to be lifted off the ground. This results in a transition zone where the characteristics of both air masses interact, often leading to precipitation and changes in weather patterns.

冷闭合锋是指一种天气锋面,当较冷的气团追赶上较暖的气团时,导致暖空气被抬升离开地面。这会形成一个过渡区域,其中两种气团的特性相互作用,通常会导致降水和天气模式的变化。

例句

1.Meteorologists predict that a cold occlusion front 冷锋闭合前线 will bring significant changes in weather patterns this weekend.

气象学家预测,一个冷锋闭合前线 cold occlusion front将在本周末带来显著的天气变化。

2.As the cold occlusion front 冷锋闭合前线 moves in, temperatures are expected to drop dramatically.

随着冷锋闭合前线 cold occlusion front的到来,气温预计将急剧下降。

3.A cold occlusion front 冷锋闭合前线 can create unstable atmospheric conditions, leading to severe weather.

一个冷锋闭合前线 cold occlusion front可以造成不稳定的大气条件,从而导致严重的天气。

4.Farmers should be aware of the approaching cold occlusion front 冷锋闭合前线 to protect their crops from frost.

农民应该注意即将到来的冷锋闭合前线 cold occlusion front,以保护他们的作物免受霜冻影响。

5.The cold occlusion front 冷锋闭合前线 can lead to heavy rainfall and thunderstorms in the affected areas.

在受影响地区,冷锋闭合前线 cold occlusion front可能导致大雨和雷暴。

作文

In meteorology, understanding different types of weather fronts is crucial for predicting weather patterns. One of the less commonly discussed fronts is the cold occlusion front, which occurs when a cold front overtakes a warm front. This phenomenon can lead to significant changes in weather conditions and is essential for meteorologists to comprehend. The cold occlusion front is characterized by the lifting of warm air over colder air masses, resulting in various weather effects. When a cold front moves into an area occupied by warmer air, it forces the warm air to rise rapidly. As this warm air ascends, it cools and condenses, forming clouds and precipitation. The result can be a variety of weather events, including thunderstorms, heavy rain, or even snow, depending on the temperature of the air involved.The dynamics of a cold occlusion front are fascinating. As the cold front catches up with the warm front, the warm air is lifted off the ground. This process can create instability in the atmosphere, leading to turbulent weather. Meteorologists often monitor these fronts closely because they can indicate severe weather conditions. For instance, as the warm air rises, it may cool enough to form cumulonimbus clouds, which are associated with thunderstorms. These storms can produce heavy rainfall, strong winds, and sometimes hail.Moreover, the presence of a cold occlusion front can affect local climates significantly. In regions where these fronts are common, residents may experience abrupt weather changes. For example, a sunny day can quickly turn into a stormy one as a cold occlusion front moves through. Understanding this concept is vital not only for meteorologists but also for everyday people who rely on weather forecasts for planning their activities.The study of cold occlusion fronts is also essential for aviation and shipping industries, as these weather changes can impact flight paths and sea routes. Pilots need to be aware of potential turbulence associated with these fronts, while ships must navigate carefully to avoid storms that can arise suddenly. Therefore, the implications of cold occlusion fronts extend beyond just daily weather; they have practical applications in various sectors.In conclusion, the cold occlusion front is a significant meteorological phenomenon that plays a crucial role in weather prediction and understanding. By recognizing the characteristics and impacts of this front, we can better prepare for the weather changes it brings. As our understanding of meteorology continues to evolve, the importance of studying different types of fronts, including the cold occlusion front, will remain a key aspect of ensuring safety and preparedness in our daily lives.

在气象学中,理解不同类型的天气锋面对于预测天气模式至关重要。其中一个不太常被讨论的锋面是冷闭合锋,它发生在冷锋追上暖锋时。这种现象可能导致天气条件的显著变化,对于气象学家来说,理解这一点是必要的。冷闭合锋的特点是暖空气在较冷的空气团上升,导致各种天气效应。当冷锋移动到暖空气占据的区域时,它迫使暖空气迅速上升。随着这股暖空气的上升,它会冷却并凝结,形成云和降水。结果可能是多种天气事件,包括雷暴、大雨,甚至是雪,这取决于涉及空气的温度。冷闭合锋的动力学非常引人入胜。当冷锋追上暖锋时,暖空气被抬离地面。这个过程可以在大气中造成不稳定,导致天气动荡。气象学家通常密切监测这些锋面,因为它们可能表明严重的天气条件。例如,当暖空气上升时,它可能会冷却到足以形成积雨云,而这些云与雷暴有关。这些风暴可能会产生强降雨、强风,有时还会伴随冰雹。此外,冷闭合锋的存在可能会显著影响当地气候。在这些锋面常见的地区,居民可能会经历突如其来的天气变化。例如,一个阳光明媚的日子可能会在冷闭合锋经过时迅速变成暴风雨。因此,理解这一概念对气象学家以及依赖天气预报进行活动规划的普通人来说都是至关重要的。冷闭合锋的研究对于航空和航运业也至关重要,因为这些天气变化可能会影响航班路线和海上航线。飞行员需要意识到与这些锋面相关的潜在湍流,而船只必须小心航行,以避免突然出现的风暴。因此,冷闭合锋的影响超出了日常天气;它在各个行业都有实际应用。总之,冷闭合锋是一个重要的气象现象,在天气预测和理解中扮演着关键角色。通过识别这种锋面的特征和影响,我们可以更好地为它带来的天气变化做好准备。随着我们对气象学理解的不断发展,研究不同类型锋面的重要性,包括冷闭合锋,将继续是确保我们日常生活安全和准备工作的关键方面。

相关单词

occlusion

occlusion详解:怎么读、什么意思、用法