anabatic wind
简明释义
上升风
英英释义
Anabatic wind is a warm, rising wind that occurs when air is heated by contact with a sloped surface, such as a mountain or hill, causing it to ascend. | 上升风是一种温暖的上升风,当空气与斜坡表面(如山或丘陵)接触时被加热,导致其上升。 |
例句
1.In mountainous regions, the anabatic wind 上升风 plays a crucial role in the ecosystem.
在山区,上升风 anabatic wind在生态系统中起着至关重要的作用。
2.During the afternoon, the sun heats the mountains, creating an anabatic wind 上升风 that rises up the slopes.
在下午,阳光加热山脉,形成一种上升风 anabatic wind,向坡面上升。
3.As we hiked higher, we felt the cool breeze of the anabatic wind 上升风 against our faces.
当我们爬得更高时,感受到来自上升风 anabatic wind的凉爽微风吹拂着我们的脸庞。
4.The meteorologist explained how the anabatic wind 上升风 contributes to local weather patterns.
气象学家解释了上升风 anabatic wind如何影响当地天气模式。
5.The anabatic wind 上升风 can enhance thermal updrafts, making it ideal for gliders.
这种上升风 anabatic wind可以增强热气流,使其非常适合滑翔机。
作文
The phenomenon of wind is a fascinating subject that has intrigued scientists and nature enthusiasts alike for centuries. Among the various types of winds, the anabatic wind (上升风) stands out due to its unique characteristics and formation process. Anabatic winds are warm, rising winds that occur when the sun heats up the slopes of mountains or hills during the day. As the air near the surface warms, it becomes less dense and starts to rise, creating a flow of air that moves upward along the terrain. This process is particularly prominent in mountainous regions, where the temperature difference between the sunlit slopes and the shaded valleys can be quite significant.In contrast to anabatic winds (上升风), we have katabatic winds, which are cold, descending winds that occur during the night when the air cools down rapidly on the slopes. This contrast between anabatic and katabatic winds illustrates the dynamic nature of atmospheric conditions and how they can change with time of day and geographical features.The effects of anabatic winds (上升风) can be observed in various ecological and meteorological contexts. For instance, these winds can enhance local weather patterns by promoting cloud formation and precipitation. As the warm air rises, it can carry moisture upwards, leading to condensation and, eventually, rainfall. This is particularly important for agriculture in mountainous areas, where water resources may be scarce. Farmers often rely on the predictable patterns of anabatic winds (上升风) for irrigation and crop growth.Additionally, anabatic winds (上升风) play a crucial role in the dispersal of seeds and pollen. The upward movement of air can help carry these biological materials to higher altitudes, facilitating the spread of plant species across different elevations. This natural process contributes to biodiversity and the resilience of ecosystems in mountainous regions.Moreover, the study of anabatic winds (上升风) is essential for understanding climate change and its impacts on local environments. As global temperatures rise, the behavior of these winds may shift, affecting weather patterns and ecosystems. Researchers are increasingly focused on monitoring these changes to predict future climatic conditions and their implications for both human and natural systems.In conclusion, anabatic winds (上升风) are more than just a meteorological curiosity; they are a vital component of our planet's climate system. Their ability to transport warm air, facilitate precipitation, and support biodiversity highlights their importance in both natural and agricultural contexts. As we continue to explore the complexities of our atmosphere, understanding phenomena like anabatic winds (上升风) will be crucial for developing effective strategies to adapt to and mitigate the impacts of climate change. By appreciating the intricacies of these winds, we can gain a deeper respect for the natural world and the delicate balance that sustains it.
风的现象是一个迷人的主题,几个世纪以来一直吸引着科学家和自然爱好者的兴趣。在各种类型的风中,anabatic wind(上升风)因其独特的特征和形成过程而脱颖而出。上升风是温暖的上升风,当太阳在白天加热山坡或丘陵时就会发生。随着靠近地面的空气变暖,它变得不那么密集并开始上升,形成沿着地形向上的气流。这一过程在山区尤为明显,因为阳光照射的坡面与阴影山谷之间的温差可能相当显著。与anabatic winds(上升风)相反,我们有下沉风(katabatic winds),它们是冷的下降风,发生在夜间,当坡面的空气迅速降温时。这种上升风和下降风之间的对比展示了大气条件的动态特性,以及它们如何随时间和地理特征而变化。anabatic winds(上升风)的影响可以在各种生态和气象背景中观察到。例如,这些风可以通过促进云的形成和降水来增强当地的天气模式。当温暖的空气上升时,它可以将水分带到更高的地方,导致凝结并最终降雨。这对于山区的农业尤其重要,因为水资源可能稀缺。农民通常依赖anabatic winds(上升风)的可预测模式进行灌溉和作物生长。此外,anabatic winds(上升风)在种子和花粉的传播中也起着至关重要的作用。空气的上升运动可以帮助将这些生物材料带到更高的海拔,从而促进植物物种在不同高度之间的传播。这一自然过程有助于生物多样性和生态系统在山区的韧性。此外,研究anabatic winds(上升风)对于理解气候变化及其对当地环境的影响至关重要。随着全球气温的上升,这些风的行为可能会发生变化,从而影响天气模式和生态系统。研究人员越来越关注监测这些变化,以预测未来气候条件及其对人类和自然系统的影响。总之,anabatic winds(上升风)不仅仅是气象学的好奇心;它们是我们星球气候系统的重要组成部分。它们运输温暖空气、促进降水和支持生物多样性的能力突显了它们在自然和农业背景中的重要性。随着我们继续探索大气的复杂性,理解像anabatic winds(上升风)这样的现象对于制定有效的应对气候变化影响的策略至关重要。通过欣赏这些风的微妙之处,我们可以更深刻地尊重自然世界及其维持的微妙平衡。
相关单词