warm air mass

简明释义

暖气团

英英释义

例句

1.A sudden shift in weather patterns can cause a large warm air mass (温暖气团) to move into the region.

天气模式的突然变化可能导致一个大型warm air mass (温暖气团) 移入该地区。

2.As the warm air mass (温暖气团) moved over the ocean, it picked up moisture and caused heavy rainfall.

当warm air mass (温暖气团) 移过海洋时，它吸收了水分并导致了大雨。

3.Meteorologists predict that the incoming warm air mass (温暖气团) will raise temperatures significantly this weekend.

气象学家预测即将到来的warm air mass (温暖气团) 将在这个周末显著提高气温。

4.The warm air mass (温暖气团) from the south is creating ideal conditions for thunderstorms.

来自南方的warm air mass (温暖气团) 正在创造理想的雷暴条件。

5.During summer, a persistent warm air mass (温暖气团) can lead to heatwaves in many areas.

在夏季，持续的warm air mass (温暖气团) 可能导致许多地区出现热浪。

作文

The phenomenon of weather is a complex interplay of various atmospheric elements, with one significant factor being the presence of a warm air mass. A warm air mass is defined as a large body of air that has relatively high temperatures compared to its surrounding environment. These air masses can significantly influence weather patterns, leading to various climatic conditions. Understanding how these warm air masses form and behave is essential for meteorologists and anyone interested in weather forecasting.Typically, warm air masses originate over warm regions such as deserts or tropical oceans. As the sun heats the surface of these areas, the air above them warms up, becoming less dense and rising into the atmosphere. This process creates a warm air mass that can travel long distances, carrying the heat with it. When a warm air mass moves into a cooler region, it can lead to various weather phenomena, including increased temperatures, changes in humidity, and even precipitation.For instance, when a warm air mass collides with a cold air mass, it can result in the formation of clouds and storms. The warm air, being lighter, rises above the cold air, creating instability in the atmosphere. This instability can lead to the development of thunderstorms, which are characterized by heavy rain, lightning, and strong winds. Therefore, understanding the behavior of warm air masses is crucial for predicting severe weather events.Moreover, warm air masses can also contribute to the phenomenon known as the urban heat island effect. In cities, where there is a concentration of buildings, roads, and other infrastructures, warm air masses can become trapped, leading to higher temperatures compared to surrounding rural areas. This can have significant implications for energy consumption, public health, and overall comfort in urban environments.In addition to their impact on local weather, warm air masses can also influence larger climatic patterns. For example, during the winter months, a persistent warm air mass can lead to milder temperatures in regions that typically experience cold weather. Conversely, during summer, the presence of a warm air mass can intensify heatwaves, leading to record-breaking temperatures.Meteorologists use advanced technology and models to track the movement and characteristics of warm air masses. By analyzing satellite imagery and weather data, they can predict how these air masses will interact with other atmospheric conditions. This information is vital for issuing weather warnings and helping communities prepare for potential impacts.In conclusion, a warm air mass plays a crucial role in shaping our weather and climate. Its formation, movement, and interaction with other air masses can lead to various weather phenomena, from sunny days to severe storms. By understanding these dynamics, we can better appreciate the complexities of our atmosphere and the importance of monitoring weather patterns. As we continue to study the effects of climate change, the role of warm air masses will remain a key area of research, influencing how we respond to future weather challenges.

天气现象是各种大气元素复杂相互作用的结果，其中一个重要因素是存在的暖空气团。暖空气团被定义为与其周围环境相比，温度相对较高的大气体块。这些空气团会显著影响天气模式，导致各种气候条件。理解这些暖空气团如何形成和变化对于气象学家和任何对天气预报感兴趣的人来说都是至关重要的。通常，暖空气团起源于温暖地区，如沙漠或热带海洋。当太阳加热这些地区的表面时，覆盖在它们上方的空气变得温暖，密度降低并向上升入大气。这一过程产生了一个可以长距离移动的暖空气团，将热量带走。当暖空气团移动到较冷区域时，会导致各种天气现象，包括温度升高、湿度变化甚至降水。例如，当一个暖空气团与一个冷空气团相遇时，可能会导致云层和风暴的形成。由于暖空气团较轻，因此会上升到冷空气之上，造成大气的不稳定。这种不稳定可能导致雷暴的发展，特征是强降雨、闪电和强风。因此，理解暖空气团的行为对于预测严重天气事件至关重要。此外，暖空气团还可能导致城市热岛效应的现象。在城市中，由于建筑物、道路和其他基础设施的集中，暖空气团可能被困住，导致与周围乡村地区相比的温度升高。这对能源消耗、公共健康和城市环境的整体舒适性具有重要影响。除了对局部天气的影响外，暖空气团还可以影响更大的气候模式。例如，在冬季，持久的暖空气团可能导致通常经历寒冷天气的地区出现温和的温度。相反，在夏季，暖空气团的存在可能会加剧热浪，导致创纪录的高温。气象学家利用先进的技术和模型来跟踪暖空气团的运动和特征。通过分析卫星图像和天气数据，他们可以预测这些空气团如何与其他大气条件相互作用。这些信息对于发布天气警报和帮助社区准备潜在影响至关重要。总之，暖空气团在塑造我们的天气和气候方面发挥着关键作用。它的形成、运动和与其他空气团的相互作用可以导致从阳光明媚的日子到严重风暴的各种天气现象。通过理解这些动态，我们可以更好地欣赏我们大气的复杂性以及监测天气模式的重要性。随着我们继续研究气候变化的影响，暖空气团的作用将仍然是研究的关键领域，影响我们应对未来天气挑战的方式。