inverted trough

简明释义

倒槽

英英释义

例句

1.During the summer, an inverted trough 倒置槽 can lead to increased humidity and thunderstorms.

在夏季，倒置槽 inverted trough可能导致湿度增加和雷暴。

2.The inverted trough 倒置槽 contributed to a significant drop in temperatures overnight.

这个倒置槽 inverted trough导致了夜间气温显著下降。

3.Farmers are concerned about the effects of the inverted trough 倒置槽 on their crops this season.

农民们担心本季倒置槽 inverted trough对他们作物的影响。

4.Travelers should be aware that an inverted trough 倒置槽 may cause flight delays due to stormy weather.

旅行者应注意，由于恶劣天气，倒置槽 inverted trough可能导致航班延误。

5.The meteorologist explained that an inverted trough 倒置槽 could bring unexpected weather changes this weekend.

气象学家解释说，一个倒置槽 inverted trough可能会在这个周末带来意想不到的天气变化。

作文

In meteorology, the term inverted trough refers to a weather phenomenon characterized by a dip in atmospheric pressure that is oriented differently from a typical trough. While a standard trough is a low-pressure area that usually extends from west to east, an inverted trough has a more unusual configuration, often bending or curving in a way that can lead to significant weather changes. Understanding this phenomenon is crucial for predicting weather patterns and preparing for potential storms. The formation of an inverted trough typically occurs when warm air rises over a cooler surface, creating a localized area of low pressure. This process can be exacerbated by geographical features such as mountains or bodies of water, which influence wind patterns and temperature distributions. As the warm air ascends, it cools and condenses, leading to the development of clouds and precipitation. This is particularly important for areas that rely on seasonal rains or are prone to droughts. Meteorologists utilize advanced technology and models to track the development of an inverted trough. Satellite imagery and radar systems provide real-time data on temperature, humidity, and wind speed, allowing forecasters to predict the movement of these troughs with greater accuracy. When an inverted trough forms, it can lead to sudden weather changes, including thunderstorms, heavy rainfall, or even tornadoes in extreme cases. For example, during the summer months, the presence of an inverted trough can lead to intense thunderstorms in the southeastern United States. The combination of warm, moist air from the Gulf of Mexico and the cooler air from the north creates a volatile environment conducive to severe weather. Residents in these areas must stay informed about weather alerts and be prepared for rapidly changing conditions. In contrast, the winter months may see different effects from an inverted trough. Cold air masses can become trapped beneath a layer of warmer air, leading to prolonged periods of cloudiness and light precipitation. This can result in overcast skies and chilly temperatures, impacting daily activities and energy consumption. In summary, the concept of an inverted trough is essential for understanding weather dynamics. Its unique characteristics can lead to various weather phenomena, significantly affecting local climates and ecosystems. By studying and monitoring these troughs, meteorologists can provide valuable information to help communities prepare for the potential impacts of severe weather. As our understanding of atmospheric processes continues to evolve, the importance of recognizing patterns such as the inverted trough will remain a critical aspect of meteorological science. In conclusion, the inverted trough serves as a reminder of the complexity of our atmosphere and the interconnectedness of various weather systems. By furthering our knowledge in this field, we can enhance our preparedness for the unpredictable nature of weather, ultimately safeguarding lives and property.

在气象学中，术语反向槽指的是一种天气现象，其特征是大气压力的下降，其方向与典型的槽不同。标准槽通常是一个从西到东延伸的低压区域，而反向槽则具有更不寻常的构造，通常弯曲或曲线，这可能导致显著的天气变化。理解这种现象对于预测天气模式和准备潜在风暴至关重要。反向槽的形成通常发生在温暖的空气上升到较冷的表面时，形成一个局部的低压区域。地理特征如山脉或水体会影响风的模式和温度分布，从而加剧这一过程。当温暖的空气上升时，它会冷却并凝结，导致云和降水的发展。这对依赖季节性降雨或易受干旱影响的地区尤为重要。气象学家利用先进的技术和模型来跟踪反向槽的发展。卫星图像和雷达系统提供实时数据，包括温度、湿度和风速，使预报员能够更准确地预测这些槽的运动。当反向槽形成时，可能导致突发的天气变化，包括雷暴、大量降雨，甚至在极端情况下出现龙卷风。例如，在夏季，反向槽的存在可能导致美国东南部的强烈雷暴。来自墨西哥湾的温暖潮湿空气与北方的冷空气相结合，创造了一个有利于严重天气的易变环境。该地区的居民必须保持关注天气预警，并为快速变化的条件做好准备。相反，冬季可能会看到反向槽的不同影响。冷空气团可能被困在一层温暖的空气下，导致持续的阴云和轻微降水。这可能导致阴天和寒冷的温度，影响日常活动和能源消耗。总之，反向槽的概念对于理解天气动态至关重要。其独特特征可能导致各种天气现象，显著影响地方气候和生态系统。通过研究和监测这些槽，气象学家可以提供有价值的信息，帮助社区为严重天气的潜在影响做好准备。随着我们对大气过程的理解不断发展，识别反向槽等模式的重要性将继续成为气象科学的关键方面。最后，反向槽提醒我们大气的复杂性以及各种天气系统之间的相互联系。通过进一步了解这一领域，我们可以增强对天气不可预测性的准备，最终保护生命和财产。