tropical upper-tropospheric trough

简明释义

热带上层对流层槽

英英释义

例句

1.The tropical upper-tropospheric trough 热带上层对流槽 was linked to the formation of several tropical storms last season.

去季节的多个热带风暴与热带上层对流槽 tropical upper-tropospheric trough有关联。

2.Understanding the dynamics of the tropical upper-tropospheric trough 热带上层对流槽 is crucial for accurate long-term weather predictions.

理解热带上层对流槽 tropical upper-tropospheric trough的动态对于准确的长期天气预报至关重要。

3.Forecast models indicated that a tropical upper-tropospheric trough 热带上层对流槽 would develop over the Caribbean next week.

预测模型显示下周将在加勒比海上方形成一个热带上层对流槽 tropical upper-tropospheric trough。

4.The presence of a tropical upper-tropospheric trough 热带上层对流槽 can lead to enhanced rainfall during the monsoon season.

一个热带上层对流槽 tropical upper-tropospheric trough的存在可能会导致季风季节降雨量增加。

5.Meteorologists observed a significant tropical upper-tropospheric trough 热带上层对流槽 that influenced the weather patterns in the region.

气象学家观察到一个显著的热带上层对流槽 tropical upper-tropospheric trough，它影响了该地区的天气模式。

作文

The atmosphere is a complex system, and understanding its various components is essential for meteorologists and climate scientists. One important feature of the atmospheric circulation is the tropical upper-tropospheric trough (TUTT), which plays a crucial role in weather patterns, particularly in tropical regions. The tropical upper-tropospheric trough (热带上层对流层槽) is a significant trough that exists in the upper levels of the troposphere, typically between 10 to 15 kilometers above sea level. This trough is characterized by a dip or trough-like formation in the upper atmosphere, which influences wind patterns and storm development in the tropics.The presence of a tropical upper-tropospheric trough (热带上层对流层槽) can lead to various weather phenomena, including the formation of tropical cyclones. When the trough is positioned correctly, it can enhance convection in the lower levels of the atmosphere, leading to increased thunderstorm activity and the potential for cyclone formation. Meteorologists closely monitor these troughs because they can significantly impact the intensity and trajectory of tropical storms and hurricanes.In addition to influencing storm development, the tropical upper-tropospheric trough (热带上层对流层槽) also affects the overall climate in tropical regions. For instance, during certain times of the year, the presence of a TUTT can lead to drier conditions in some areas while promoting rainfall in others. This variability can have profound effects on agriculture, water supply, and even local ecosystems. Understanding how the tropical upper-tropospheric trough (热带上层对流层槽) interacts with other atmospheric systems is vital for predicting weather patterns and preparing for potential natural disasters.Moreover, the tropical upper-tropospheric trough (热带上层对流层槽) is not static; it can shift and change position depending on various climatic factors, including sea surface temperatures and atmospheric pressure systems. These changes can result in significant shifts in weather patterns, making it imperative for researchers to study the dynamics of TUTTs and their interactions with other meteorological phenomena. Advances in satellite technology and numerical weather prediction models have enhanced our ability to track and predict the behavior of tropical upper-tropospheric troughs (热带上层对流层槽), providing critical information for disaster preparedness and response efforts.In conclusion, the tropical upper-tropospheric trough (热带上层对流层槽) is a vital component of the Earth's atmospheric system, significantly influencing weather patterns and climate in tropical regions. Its role in the development of tropical cyclones and its impact on local weather variability highlight the importance of understanding this phenomenon. As climate change continues to affect global weather patterns, studying the tropical upper-tropospheric trough (热带上层对流层槽) will be increasingly important for predicting future weather events and mitigating their impacts on communities around the world.

大气是一个复杂的系统，理解其各种组成部分对气象学家和气候科学家至关重要。大气环流的一个重要特征是热带上层对流层槽（TUTT），它在天气模式中扮演着关键角色，特别是在热带地区。热带上层对流层槽（热带上层对流层槽）是一个显著的槽，存在于对流层的上层，通常位于海平面以上10到15公里之间。这个槽的特征是在上层大气中形成一个凹陷或槽状结构，这影响了风模式和热带地区的风暴发展。热带上层对流层槽（热带上层对流层槽）的存在可以导致各种气象现象，包括热带气旋的形成。当这个槽的位置合适时，它可以增强大气下层的对流，导致雷暴活动增加，并有可能形成气旋。气象学家密切监测这些槽，因为它们可以显著影响热带风暴和飓风的强度和轨迹。除了影响风暴发展之外，热带上层对流层槽（热带上层对流层槽）还影响热带地区的整体气候。例如，在某些季节，TUTT的存在可能导致某些地区干燥，而在其他地区促进降雨。这种变异性对农业、水供应甚至地方生态系统都有深远的影响。理解热带上层对流层槽（热带上层对流层槽）如何与其他大气系统相互作用对于预测天气模式和为潜在自然灾害做好准备至关重要。此外，热带上层对流层槽（热带上层对流层槽）并不是静态的；它可以根据各种气候因素，包括海面温度和大气压力系统而移动和改变位置。这些变化可能导致天气模式的显著变化，使研究人员必须研究TUTT的动态及其与其他气象现象的相互作用。卫星技术和数值天气预报模型的进步增强了我们追踪和预测热带上层对流层槽（热带上层对流层槽）行为的能力，为灾害准备和响应工作提供了重要信息。总之，热带上层对流层槽（热带上层对流层槽）是地球大气系统的重要组成部分，对热带地区的天气模式和气候产生重大影响。它在热带气旋发展中的作用以及对地方天气变异性的影响突显了理解这一现象的重要性。随着气候变化继续影响全球天气模式，研究热带上层对流层槽（热带上层对流层槽）将对预测未来天气事件及减轻其对全球各地社区影响的重要性日益增加。