transcontinental air-mass

简明释义

横跨大陆气团

英英释义

A transcontinental air-mass refers to a large body of air that extends across an entire continent, characterized by relatively uniform temperature and humidity properties.

跨大陆气团是指一个覆盖整个大陆的大气体,具有相对均匀的温度和湿度特性。

例句

1.Meteorologists study the transcontinental air-mass 跨洲气团 patterns to better understand climate change effects.

气象学家研究跨洲气团 transcontinental air-mass模式,以更好地理解气候变化的影响。

2.During summer, the transcontinental air-mass 跨洲气团 can influence thunderstorms in various regions.

在夏季,跨洲气团 transcontinental air-mass可能会影响各个地区的雷暴天气。

3.The forecast predicts a shift in the transcontinental air-mass 跨洲气团, bringing warmer temperatures to the Midwest.

天气预报预测,跨洲气团 transcontinental air-mass的变化将使中西部地区气温上升。

4.Changes in the transcontinental air-mass 跨洲气团 can lead to severe drought conditions in some areas.

在某些地区,跨洲气团 transcontinental air-mass的变化可能导致严重干旱。

5.A strong transcontinental air-mass 跨洲气团 has moved across the Atlantic, causing unusual weather in Europe.

一股强大的跨洲气团 transcontinental air-mass已穿越大西洋,导致欧洲出现异常天气。

作文

The concept of a transcontinental air-mass refers to a large body of air that extends across multiple continents, significantly influencing the weather patterns in the regions it affects. Understanding this phenomenon is crucial for meteorologists and climate scientists, as it helps them predict weather changes and understand climatic variations. A transcontinental air-mass can originate from various geographical areas, such as polar regions or tropical zones, and its characteristics depend on the source region from which it develops.For instance, an air mass that forms over the Arctic region is typically cold and dry, whereas one that originates over the Gulf of Mexico is warm and humid. When these transcontinental air-masses travel across different terrains, they interact with local weather systems, leading to various meteorological events. This interaction can result in thunderstorms, heavy rainfall, or even droughts, depending on the nature of the air mass and the geographical features it encounters.One significant example of a transcontinental air-mass is the North American air mass that moves from the Pacific Ocean across the continent to the Atlantic. As it travels, it picks up moisture from the ocean, which can lead to precipitation when it reaches land. This process is vital for replenishing freshwater resources in many areas, highlighting the importance of understanding transcontinental air-masses in relation to water cycles.In addition to their role in precipitation, transcontinental air-masses also play a critical role in temperature regulation. For instance, when a cold transcontinental air-mass moves southward, it can bring unseasonably low temperatures to regions that are typically warmer. Conversely, a warm transcontinental air-mass moving north can lead to heatwaves in areas that usually experience milder conditions. These temperature shifts can have significant impacts on agriculture, energy consumption, and overall ecosystem health.Moreover, the study of transcontinental air-masses is essential for climate change research. As global temperatures rise, the behavior of these air masses may alter, leading to unpredictable weather patterns. For example, scientists are observing changes in the frequency and intensity of storms associated with transcontinental air-masses, which could be linked to climate change. This makes it imperative for researchers to monitor these systems closely and understand their dynamics.In conclusion, the term transcontinental air-mass encompasses a vital aspect of meteorology that affects weather patterns, temperature regulation, and precipitation. By studying these air masses, scientists can gain insights into weather forecasting and climate change, ultimately helping societies prepare for and adapt to changing environmental conditions. The significance of transcontinental air-masses extends beyond mere academic interest; it has real-world implications for agriculture, water resources, and disaster management. Therefore, a deeper understanding of these phenomena is essential for building resilience against the challenges posed by our ever-changing climate.

“跨洲气团”这一概念指的是一种横跨多个大陆的大型气团,显著影响其所影响区域的天气模式。理解这一现象对气象学家和气候科学家至关重要,因为它帮助他们预测天气变化并了解气候变化。一个“跨洲气团”可以源自不同的地理区域,例如极地或热带区域,其特征取决于其形成的源区域。例如,形成于北极地区的气团通常是寒冷且干燥的,而起源于墨西哥湾的气团则是温暖且潮湿的。当这些“跨洲气团”穿越不同的地形时,它们与当地的天气系统相互作用,从而导致各种气象事件。这种相互作用可能导致雷暴、大雨甚至干旱,具体取决于气团的性质及其所遇到的地理特征。一个“跨洲气团”的显著例子是从太平洋移动到大西洋的北美气团。当它移动时,它从海洋中吸收水分,当它到达陆地时可能会导致降水。这一过程对于补充许多地区的淡水资源至关重要,突显了理解“跨洲气团”与水循环关系的重要性。除了在降水中的作用外,“跨洲气团”在温度调节中也发挥着关键作用。例如,当一个寒冷的“跨洲气团”向南移动时,它可能会给通常较温暖的区域带来不合季节的低温。相反,一个向北移动的温暖“跨洲气团”可能会导致通常气候较温和的地区出现热浪。这些温度变化可能对农业、能源消费和整体生态系统健康产生重大影响。此外,“跨洲气团”的研究对于气候变化研究至关重要。随着全球气温上升,这些气团的行为可能会发生变化,导致不可预测的天气模式。例如,科学家观察到与“跨洲气团”相关的风暴频率和强度的变化,可能与气候变化有关。这使得研究人员必须密切监测这些系统并理解其动态。总之,“跨洲气团”这一术语涵盖了气象学的一个重要方面,影响着天气模式、温度调节和降水。通过研究这些气团,科学家可以深入了解天气预报和气候变化,最终帮助社会为应对不断变化的环境条件做好准备。理解“跨洲气团”的重要性不仅仅是学术兴趣;它对农业、水资源和灾害管理具有实际意义。因此,深入理解这些现象对于增强应对我们不断变化的气候所带来的挑战的韧性至关重要。