supersaturated air

简明释义

过饱和空气

英英释义

例句

1.Understanding the dynamics of supersaturated air (过饱和空气) is crucial for predicting weather patterns.

理解过饱和空气（过饱和空气）的动态对于预测天气模式至关重要。

2.During a storm, the atmosphere is often filled with supersaturated air (过饱和空气), which can lead to heavy rainfall.

在暴风雨期间，大气中常常充满过饱和空气（过饱和空气），这可能导致大雨倾盆而下。

3.In meteorology, when the temperature drops, the humidity can lead to the formation of clouds in supersaturated air (过饱和空气).

在气象学中，当温度下降时，湿度可能导致在过饱和空气（过饱和空气）中形成云。

4.The condensation process occurs when supersaturated air (过饱和空气) cools down rapidly.

当过饱和空气（过饱和空气）迅速降温时，凝结过程就会发生。

5.Fog forms in supersaturated air (过饱和空气) when tiny water droplets remain suspended in the atmosphere.

当微小水滴悬浮在大气中时，雾会在过饱和空气（过饱和空气）中形成。

作文

The phenomenon of supersaturated air is a fascinating aspect of atmospheric science that plays a significant role in various weather patterns and processes. To understand this concept, we must first look at the basics of saturation in the air. Saturation occurs when the air holds the maximum amount of water vapor it can contain at a given temperature and pressure. When air is saturated, it is at 100% relative humidity, meaning it cannot hold any more moisture without some of it condensing into liquid water. However, under certain conditions, air can hold more moisture than this saturation point, leading to the state known as supersaturated air (过饱和空气). This condition typically arises when air is cooled rapidly or when it is mixed with other air masses that have different humidity levels.One common example of supersaturated air occurs in the formation of clouds. As warm, moist air rises, it expands and cools due to lower atmospheric pressure at higher altitudes. If this cooling happens quickly enough, the air can become supersaturated air (过饱和空气), allowing water vapor to remain in the gaseous state even beyond its saturation point. Eventually, this excess moisture condenses around tiny particles in the atmosphere, such as dust or pollen, forming cloud droplets. This process is crucial for cloud formation and precipitation, illustrating how supersaturated air (过饱和空气) contributes to the water cycle.Another interesting aspect of supersaturated air is its role in weather phenomena like fog and dew. Fog often forms when warm, moist air comes into contact with cooler surfaces, leading to rapid cooling and the creation of supersaturated air (过饱和空气). The moisture in the supersaturated air (过饱和空气) then condenses into tiny water droplets, creating the dense mist that characterizes foggy conditions. Similarly, dew forms during the night when temperatures drop, causing the air near the ground to become supersaturated air (过饱和空气), resulting in condensation on surfaces like grass and leaves.In addition to its impact on weather, supersaturated air (过饱和空气) is also important in various industrial and scientific applications. For instance, in the field of meteorology, understanding supersaturated air (过饱和空气) helps scientists predict storms and rainfall patterns. In the food industry, supersaturated air (过饱和空气) is utilized in processes like drying and preserving foods, where controlling humidity levels is essential for maintaining quality.Overall, the study of supersaturated air (过饱和空气) reveals the complexities of our atmosphere and its behaviors. By grasping the principles behind this phenomenon, we can better understand not only weather patterns but also the broader implications for our environment and industries. The interplay between temperature, pressure, and moisture content creates a dynamic system where supersaturated air (过饱和空气) is both a natural occurrence and a critical factor in various processes. As we continue to explore and learn about our atmosphere, the significance of supersaturated air (过饱和空气) will undoubtedly remain a key topic in both scientific research and practical applications.

过饱和空气现象是大气科学中一个迷人的方面，在各种天气模式和过程中发挥着重要作用。要理解这一概念，我们首先必须了解空气饱和的基本知识。当空气在给定温度和压力下保持最大水蒸气量时，就会发生饱和现象。当空气饱和时，相对湿度为100%，这意味着它不能再容纳更多水分，除非部分水分凝结成液态水。然而，在某些条件下，空气可以超过这一饱和点，导致称为过饱和空气（supersaturated air）的状态。这种情况通常发生在空气迅速冷却或与具有不同湿度水平的其他空气团混合时。过饱和空气的一个常见例子发生在云的形成过程中。当温暖潮湿的空气上升时，由于高海拔地区气压较低，它会膨胀并冷却。如果这种冷却发生得足够快，空气可能会变成过饱和空气（supersaturated air），使得水蒸气即使超过其饱和点仍保持气态。最终，这些多余的水分会围绕大气中的微小颗粒（如灰尘或花粉）凝结，形成云滴。这个过程对于云的形成和降水至关重要，说明了过饱和空气（supersaturated air）如何促进水循环。过饱和空气的另一个有趣方面是其在雾和露水等天气现象中的作用。当温暖潮湿的空气接触到较凉的表面时，往往会形成雾，导致快速冷却并产生过饱和空气（supersaturated air）。过饱和空气中的水分（supersaturated air）随后会凝结成微小的水滴，形成特征性的浓雾。同样，露水是在夜间形成的，当温度下降时，靠近地面的空气变得过饱和空气（supersaturated air），导致在草叶等表面上的凝结。除了对天气的影响，过饱和空气（supersaturated air）在各种工业和科学应用中也很重要。例如，在气象学领域，理解过饱和空气（supersaturated air）帮助科学家预测风暴和降雨模式。在食品行业，过饱和空气（supersaturated air）被用于干燥和保存食品的过程中，其中控制湿度水平对于保持质量至关重要。总体而言，研究过饱和空气（supersaturated air）揭示了我们大气及其行为的复杂性。通过掌握这一现象背后的原理，我们可以更好地理解天气模式以及对环境和工业的更广泛影响。温度、压力和湿度含量之间的相互作用创造了一个动态系统，其中过饱和空气（supersaturated air）既是自然现象，也是各种过程中的关键因素。随着我们继续探索和学习我们的气候，过饱和空气（supersaturated air）的重要性无疑将继续成为科学研究和实际应用中的一个关键主题。