air mass temperature

简明释义

气团温度

英英释义

例句

1.Changes in air mass temperature 气团温度 are critical for storm development.

气团温度的变化对风暴的发展至关重要。

2.Understanding the air mass temperature 气团温度 helps in predicting weather patterns.

理解气团温度有助于预测天气模式。

3.The meteorologist reported that the air mass temperature 气团温度 would significantly drop overnight.

气象学家报告说，气团温度将在夜间显著下降。

4.A warm front is often associated with a rise in air mass temperature 气团温度.

暖锋通常与气团温度的上升有关。

5.The air mass temperature 气团温度 can influence local climate conditions.

气团温度可以影响当地气候条件。

作文

Understanding the concept of air mass temperature is crucial for anyone interested in meteorology or climate science. An air mass temperature refers to the temperature of a large body of air that has similar properties throughout. These air masses can form over various geographical areas and are influenced by the underlying surface, whether it be land or water. For instance, an air mass that forms over the ocean tends to have a different temperature than one that forms over a desert. This difference is essential because it affects weather patterns and climatic conditions across regions.When discussing air mass temperature, it is important to consider how these temperatures can change due to various factors. The time of year plays a significant role; during summer months, air masses over land can heat up significantly, while those over water remain relatively cooler. Conversely, during winter, the opposite can occur, with land-based air masses cooling down more rapidly than those over oceans. This disparity can lead to various weather phenomena, such as thunderstorms, hurricanes, or even droughts, depending on the interactions between different air masses.Meteorologists often categorize air masses based on their source regions and their air mass temperature. There are four primary types: continental polar (cP), maritime polar (mP), continental tropical (cT), and maritime tropical (mT). Each of these air masses has distinct temperature characteristics and moisture levels, which influence the weather patterns they bring. For example, a continental tropical air mass is typically hot and dry, while a maritime tropical air mass is warm and moist. Understanding these classifications helps in predicting weather changes and preparing for severe weather events.The movement of air masses also plays a vital role in determining the air mass temperature experienced in a particular area. When air masses move, they can collide and interact with each other, leading to changes in temperature and precipitation. For instance, when a cold front from a polar air mass meets a warm, moist air mass from the tropics, it can create significant weather changes, such as storms or heavy rainfall. This interaction is crucial for understanding regional climates and forecasting weather.Additionally, the concept of air mass temperature is not just limited to temperature alone but also encompasses the idea of stability and instability within the atmosphere. Stable air masses tend to resist vertical motion, which can lead to clear skies and calm weather. On the other hand, unstable air masses can rise and create clouds, precipitation, and storms. This dynamic is critical for meteorologists as they analyze weather systems and make predictions about future weather conditions.In conclusion, mastering the concept of air mass temperature is essential for understanding weather patterns and climate dynamics. By studying how air masses form, move, and interact, we can gain insights into the complexities of our atmosphere. Whether you are a student, a professional in the field, or simply an enthusiast, recognizing the significance of air mass temperature will enhance your appreciation of the ever-changing nature of our weather. As we continue to face challenges related to climate change, understanding these fundamental concepts will become increasingly important for preparing for and adapting to our changing environment.

理解气团温度的概念对任何对气象或气候科学感兴趣的人来说都是至关重要的。气团温度是指一个大型气团的温度，该气团在整个区域内具有相似的特性。这些气团可以在不同的地理区域形成，并受到底层表面的影响，无论是陆地还是水域。例如，形成于海洋上的气团往往与形成于沙漠上的气团温度不同。这种差异是重要的，因为它会影响各个地区的天气模式和气候条件。在讨论气团温度时，考虑这些温度如何因各种因素而变化是很重要的。季节的时间起着重要作用；在夏季，陆地上的气团可以显著升温，而水面上的气团则保持相对较凉。相反，在冬季，情况可能会相反，陆基气团比海洋上的气团降温更快。这种差异可能导致各种天气现象，如雷暴、飓风甚至干旱，这取决于不同气团之间的相互作用。气象学家通常根据气团的源区域及其气团温度对气团进行分类。主要有四种类型：大陆极地(cP)、海洋极地(mP)、大陆热带(cT)和海洋热带(mT)。每种气团都有独特的温度特征和湿度水平，这些特征会影响它们带来的天气模式。例如，大陆热带气团通常是炎热和干燥的，而海洋热带气团则是温暖和潮湿的。理解这些分类有助于预测天气变化并为严重天气事件做好准备。气团的移动也在决定特定区域的气团温度方面发挥着重要作用。当气团移动时，它们可以相互碰撞并相互作用，导致温度和降水的变化。例如，当来自极地气团的冷锋与来自热带的温暖潮湿气团相遇时，可能会造成显著的天气变化，如风暴或大雨。这种相互作用对于理解区域气候和天气预报至关重要。此外，气团温度的概念不仅仅局限于温度本身，还包括大气中稳定性和不稳定性的概念。稳定的气团往往抵抗垂直运动，这可能导致晴朗的天空和宁静的天气。另一方面，不稳定的气团可以上升并形成云、降水和风暴。这个动态对于气象学家来说至关重要，因为他们分析天气系统并预测未来的天气条件。总之，掌握气团温度的概念对理解天气模式和气候动态至关重要。通过研究气团是如何形成、移动和相互作用的，我们可以深入了解我们大气的复杂性。无论您是学生、专业人士还是单纯的爱好者，认识到气团温度的重要性将增强您对我们不断变化的天气的欣赏。随着我们继续面临与气候变化相关的挑战，理解这些基本概念将变得越来越重要，以便为我们的变化环境做好准备和适应。