tropical continental air
简明释义
热带大陆气团
英英释义
Tropical continental air refers to a type of air mass that forms over land in tropical regions, characterized by warm temperatures and low humidity. | 热带大陆气团是指在热带地区陆地上形成的一种气团,特点是温度较高且湿度较低。 |
例句
1.Travelers should be prepared for the heat brought by tropical continental air 热带大陆空气 when visiting the region in July.
在七月访问该地区时,旅行者应为热带大陆空气 热带大陆空气带来的高温做好准备。
2.During summer, the city often experiences warm winds from tropical continental air 热带大陆空气, making it feel much hotter.
在夏季,这座城市经常受到来自热带大陆空气 热带大陆空气的暖风影响,使得体感温度大幅上升。
3.The weather forecast predicts that the region will experience a surge of tropical continental air 热带大陆空气, leading to higher temperatures this weekend.
天气预报预测该地区将经历一股热带大陆空气 热带大陆空气,这将导致本周末气温升高。
4.The meteorologist explained how tropical continental air 热带大陆空气 interacts with other air masses to create thunderstorms.
气象学家解释了热带大陆空气 热带大陆空气是如何与其他气团相互作用以产生雷暴的。
5.Farmers are concerned that the arrival of tropical continental air 热带大陆空气 could dry out their crops.
农民们担心热带大陆空气 热带大陆空气的到来可能会使他们的作物干枯。
作文
The climate of our planet is shaped by a variety of air masses, each with its own characteristics and influences. One such air mass is known as tropical continental air, which plays a significant role in the weather patterns of certain regions. This type of air mass originates over land in tropical areas, leading to distinct features that can affect local climates profoundly. Understanding tropical continental air is essential for meteorologists and anyone interested in climate science.To begin with, tropical continental air is characterized by its warm temperatures and low humidity. Because it forms over land rather than over water, it lacks the moisture that is typically found in maritime air masses. As a result, when tropical continental air moves into an area, it can lead to dry conditions, especially during the summer months. This phenomenon is particularly noticeable in regions such as the southwestern United States, where this air mass can contribute to drought conditions.In addition to its dryness, tropical continental air can also lead to significant temperature variations. During the day, areas influenced by this air mass can experience intense heat, while nighttime temperatures may drop considerably. This diurnal temperature variation is due to the lack of moisture in the air, which allows for rapid cooling after sunset. Such conditions can create challenges for agriculture, as crops may become stressed from the heat during the day and then face cold temperatures at night.Furthermore, the interaction between tropical continental air and other air masses can lead to various weather phenomena. For instance, when this warm, dry air meets cooler, moist air from the ocean, it can create instability in the atmosphere. This instability can result in thunderstorms, particularly in transitional seasons like spring and fall. These storms can be severe, bringing heavy rainfall and even hail, which can be damaging to both natural ecosystems and human infrastructure.Moreover, tropical continental air can influence the formation of high-pressure systems. When this air mass settles over a region, it can lead to stable weather conditions, often resulting in clear skies and sunny days. However, prolonged periods of high pressure can also result in heat waves, which pose health risks to vulnerable populations.In conclusion, understanding tropical continental air is crucial for predicting weather patterns and preparing for the impacts of climate variability. Its characteristics—warmth, dryness, and potential for extreme temperature changes—make it a unique and important air mass in meteorology. By studying how tropical continental air interacts with other air masses and geographical features, scientists can improve their forecasts and help communities prepare for the effects of changing weather conditions. As climate change continues to alter weather patterns globally, the role of tropical continental air will likely become even more significant, highlighting the need for ongoing research and understanding in this field.
我们星球的气候受到多种气团的影响,每种气团都有其独特的特征和影响。其中一种气团被称为热带大陆气团,它在某些地区的天气模式中发挥着重要作用。这种气团起源于热带地区的陆地,导致其具有明显的特征,能够深刻影响当地气候。理解热带大陆气团对于气象学家和任何对气候科学感兴趣的人来说都是至关重要的。首先,热带大陆气团的特点是温暖的温度和低湿度。由于它是在陆地上形成,而不是在水面上形成,它缺乏海洋气团通常存在的湿气。因此,当热带大陆气团移动到一个地区时,尤其是在夏季,它可能导致干燥的条件。这种现象在美国西南部等地区尤为明显,在这些地区,这种气团可能会导致干旱条件。除了干燥外,热带大陆气团还可能导致显著的温度变化。在受这种气团影响的地区,白天的温度可以非常高,而夜间的温度可能会显著下降。这种日夜温差是由于空气中的湿气缺乏,使得日落后迅速降温。这种条件可能给农业带来挑战,因为作物在白天可能因高温而受到压力,而在夜间又面临寒冷的温度。此外,热带大陆气团与其他气团的相互作用可以导致各种天气现象。例如,当这种温暖、干燥的空气与来自海洋的凉爽、潮湿的空气相遇时,可能会在大气中产生不稳定性。这种不稳定性可能导致雷暴,特别是在春秋等过渡季节。这些风暴可能是严重的,带来大量降雨甚至冰雹,这可能对自然生态系统和人类基础设施造成破坏。此外,热带大陆气团还可能影响高压系统的形成。当这种气团停留在一个地区时,可能导致稳定的天气条件,通常会导致晴朗的天空和阳光明媚的日子。然而,长期的高压也可能导致热浪,对脆弱人群构成健康风险。总之,理解热带大陆气团对于预测天气模式和为气候变化的影响做好准备至关重要。它的特征——温暖、干燥和极端温度变化的潜力——使其成为气象学中独特而重要的气团。通过研究热带大陆气团如何与其他气团和地理特征相互作用,科学家们可以提高他们的天气预报能力,并帮助社区为气候条件变化的影响做好准备。随着气候变化继续改变全球天气模式,热带大陆气团的角色可能变得更加重要,这突显了这一领域需要持续研究和理解。
相关单词