continental tropical air mass

简明释义

大陆性热带气团

英英释义

例句

1.Meteorologists predict that a continental tropical air mass (大陆热带气团) will move into the region, increasing the likelihood of heatwaves.

气象学家预测一个大陆热带气团将移动到该地区，增加热浪的可能性。

2.Farmers need to be cautious when a continental tropical air mass (大陆热带气团) settles over their crops, as it can create drought conditions.

当一个大陆热带气团覆盖他们的作物时，农民需要小心，因为这可能造成干旱条件。

3.During the summer, a strong continental tropical air mass (大陆热带气团) can lead to extremely high temperatures in the southwestern United States.

在夏季，强烈的大陆热带气团会导致美国西南部极高的温度。

4.The transition from a continental tropical air mass (大陆热带气团) to a maritime polar air mass can cause severe thunderstorms.

从大陆热带气团转变为海洋极地气团可能会引发严重的雷暴。

5.The presence of a continental tropical air mass (大陆热带气团) often results in dry conditions and high humidity levels.

一个大陆热带气团的存在通常会导致干燥的天气和高湿度水平。

作文

Understanding weather patterns is crucial for predicting climate changes and preparing for natural disasters. One of the fundamental concepts in meteorology is the air mass, which refers to a large body of air that possesses uniform temperature and humidity characteristics. Among the various types of air masses, the continental tropical air mass plays a significant role in influencing weather conditions, particularly in regions like the southwestern United States and northern Mexico. This type of air mass originates over land in tropical regions, where it absorbs heat and moisture from the warm ground. As a result, the continental tropical air mass is typically warm and dry. When this air mass moves into areas with cooler temperatures, it can lead to dramatic weather changes. For instance, when a continental tropical air mass interacts with a colder front, it can create thunderstorms and severe weather conditions. These storms are often characterized by heavy rainfall, lightning, and even tornadoes. Understanding the behavior of the continental tropical air mass is essential for meteorologists to issue accurate weather forecasts and warnings.The impact of a continental tropical air mass is not limited to just precipitation. It also affects temperature and humidity levels in the regions it traverses. Areas influenced by this air mass tend to experience hot and dry weather during the summer months, leading to drought conditions if prolonged. Conversely, when this air mass collides with other weather systems, it can lead to sudden and intense rain events, which may cause flooding in previously dry areas.In addition to its effects on local weather, the continental tropical air mass also contributes to larger climatic patterns. For example, during the summer, the presence of this air mass can enhance the development of tropical cyclones in adjacent oceanic regions. The warm, moist air from the ocean can interact with the hot, dry air from the continental tropical air mass, creating conditions conducive to storm formation.Moreover, understanding the dynamics of the continental tropical air mass is vital for agriculture in affected regions. Farmers need to be aware of the potential for drought or sudden rainstorms to plan their planting and harvesting schedules effectively. The influence of this air mass on soil moisture and temperature can significantly affect crop yields and overall agricultural productivity.In conclusion, the continental tropical air mass is a critical component of our weather systems, influencing everything from daily weather patterns to long-term climate trends. By studying the characteristics and behaviors of this air mass, meteorologists can provide valuable insights into weather forecasting, disaster preparedness, and agricultural planning. As our climate continues to change, understanding the role of different air masses, including the continental tropical air mass, will become increasingly important for adapting to new weather realities and mitigating the impacts of climate change.

理解天气模式对于预测气候变化和准备自然灾害至关重要。气象学中的一个基本概念是气团，它指的是一个具有均匀温度和湿度特征的大气体。在各种类型的气团中，大陆热带气团在影响天气条件方面发挥着重要作用，特别是在美国西南部和墨西哥北部等地区。这种类型的气团起源于热带地区的陆地，在那里它从温暖的地面吸收热量和湿气。因此，大陆热带气团通常是温暖而干燥的。当这个气团移动到温度较低的地区时，会导致剧烈的天气变化。例如，当大陆热带气团与冷锋相互作用时，会产生雷暴和严重的天气条件。这些风暴通常以强降雨、闪电甚至龙卷风为特征。理解大陆热带气团的行为对于气象学家发出准确的天气预报和警报至关重要。大陆热带气团的影响不仅限于降水。它还会影响经过地区的温度和湿度水平。受此气团影响的地区在夏季往往经历炎热和干燥的天气，如果持续时间过长，可能导致干旱。相反，当这个气团与其他天气系统相撞时，可能会导致突发的强降雨事件，从而在之前干燥的地区造成洪水。除了对局部天气的影响外，大陆热带气团还对更大气候模式做出贡献。例如，在夏季，这个气团的存在可以增强相邻海洋区域热带气旋的发展。来自海洋的温暖潮湿空气与大陆热带气团的炎热干燥空气相互作用，创造出有利于风暴形成的条件。此外，理解大陆热带气团的动态对于受影响地区的农业至关重要。农民需要意识到干旱或突发暴雨的潜在性，以有效规划他们的种植和收获时间表。这个气团对土壤湿度和温度的影响可以显著影响作物产量和整体农业生产力。总之，大陆热带气团是我们天气系统的一个关键组成部分，影响着从日常天气模式到长期气候趋势的一切。通过研究这种气团的特征和行为，气象学家可以为天气预报、灾难准备和农业规划提供有价值的见解。随着我们的气候持续变化，理解不同气团的角色，包括大陆热带气团，将变得越来越重要，以适应新的天气现实并减轻气候变化的影响。