wet adiabatic

简明释义

湿绝热

英英释义

例句

1.Understanding the wet adiabatic 湿绝热 process helps in forecasting severe weather events.

理解湿绝热过程有助于预测严重天气事件。

2.The concept of wet adiabatic 湿绝热 lapse rate is crucial in meteorology for predicting cloud formation.

湿绝热递减率的概念在气象学中对于预测云的形成至关重要。

3.The wet adiabatic 湿绝热 lapse rate is approximately 6°C per kilometer in the atmosphere.

湿绝热递减率在大气中大约是每公里6°C。

4.In tropical regions, the wet adiabatic 湿绝热 rate can influence the intensity of thunderstorms.

在热带地区，湿绝热率可以影响雷暴的强度。

5.When air rises, it cools at the wet adiabatic 湿绝热 rate, leading to condensation and precipitation.

当空气上升时，它以湿绝热率冷却，导致凝结和降水。

作文

The concept of wet adiabatic processes is essential in understanding atmospheric dynamics and weather patterns. In meteorology, the term wet adiabatic refers to the rate at which a saturated air parcel cools as it rises in the atmosphere. This cooling occurs due to the expansion of the air as it ascends, leading to a drop in temperature. However, unlike dry air, saturated air contains water vapor, which plays a crucial role in this process. When the air rises and cools, the water vapor condenses into clouds and precipitation, releasing latent heat. This release of heat is significant because it affects the temperature of the surrounding air, making the wet adiabatic lapse rate generally less steep than the dry adiabatic lapse rate.Understanding the wet adiabatic lapse rate is vital for predicting weather phenomena such as thunderstorms and cyclones. For instance, when warm, moist air rises, it cools at the wet adiabatic rate of approximately 6 degrees Celsius per kilometer, instead of the 10 degrees Celsius per kilometer observed in dry air. This difference can lead to the development of significant weather systems. Meteorologists use this knowledge to forecast storms and understand the formation of clouds.Moreover, the wet adiabatic process is not only crucial for weather prediction but also for climate studies. The interaction between rising air and moisture influences climate patterns across the globe. Areas near the equator, where warm air rises consistently, often experience heavy rainfall due to the wet adiabatic cooling process. Conversely, regions that do not receive moist air may remain arid and dry, illustrating the importance of this concept in climatology.In practical applications, pilots and engineers must also consider the wet adiabatic lapse rate when designing aircraft and planning flights. Understanding how air behaves at different altitudes can help in avoiding turbulence associated with rising moist air. Additionally, in the field of environmental science, the wet adiabatic process is critical in understanding how pollution disperses in the atmosphere, as moist air can carry pollutants further than dry air.In conclusion, the wet adiabatic concept is fundamental in various fields, from meteorology to aviation and environmental science. Its implications on weather prediction, climate understanding, and even engineering make it a vital area of study. As we continue to explore the complexities of our atmosphere, grasping the nuances of the wet adiabatic process will undoubtedly enhance our ability to predict and respond to weather-related challenges. The interplay between moisture, temperature, and air movement shapes not only our weather but also our environment, highlighting the importance of this scientific principle.

“湿绝热”过程的概念在理解大气动态和天气模式中至关重要。在气象学中，术语“湿绝热”指的是饱和空气团在大气中上升时冷却的速率。这种冷却是由于空气在上升过程中膨胀，导致温度下降。然而，与干燥空气不同，饱和空气含有水蒸气，这在这个过程中起着至关重要的作用。当空气上升并冷却时，水蒸气凝结成云和降水，释放出潜热。热量的释放是显著的，因为它影响周围空气的温度，使得“湿绝热”温度递减率通常比干绝热递减率更平缓。理解“湿绝热”递减率对于预测诸如雷暴和气旋等天气现象至关重要。例如，当温暖潮湿的空气上升时，它以大约每公里6摄氏度的“湿绝热”速率冷却，而不是在干燥空气中观察到的每公里10摄氏度。这种差异可能导致显著天气系统的发展。气象学家利用这一知识来预测风暴和理解云的形成。此外，“湿绝热”过程不仅对天气预测至关重要，也对气候研究至关重要。上升空气与水分的相互作用影响全球气候模式。赤道附近的地区，由于温暖的空气持续上升，往往经历大量降雨，这归因于“湿绝热”冷却过程。相反，不接收潮湿空气的地区可能保持干旱，说明这一概念在气候学中的重要性。在实际应用中，飞行员和工程师在设计飞机和规划航班时也必须考虑“湿绝热”递减率。理解不同高度空气的行为可以帮助避免与上升潮湿空气相关的湍流。此外，在环境科学领域，“湿绝热”过程对于理解污染物在大气中的扩散至关重要，因为潮湿空气可以将污染物传播得比干燥空气更远。总之，“湿绝热”概念在气象学、航空和环境科学等多个领域中都是基础。它对天气预测、气候理解甚至工程设计的影响使其成为一个重要的研究领域。随着我们继续探索大气的复杂性，掌握“湿绝热”过程的细微差别无疑将增强我们预测和应对天气相关挑战的能力。水分、温度和空气运动之间的相互作用不仅塑造了我们的天气，也塑造了我们的环境，突显了这一科学原则的重要性。