anticyclone divergence

简明释义

反气旋辐散

英英释义

例句

1.The study focused on how anticyclone divergence 反气旋发散 affects air quality in urban environments.

这项研究集中于反气旋发散如何影响城市环境中的空气质量。

2.The weather forecast indicated that the region would experience significant anticyclone divergence 反气旋发散 this weekend, leading to clear skies.

天气预报显示，该地区本周末将经历显著的反气旋发散，导致天空晴朗。

3.During summer, the anticyclone divergence 反气旋发散 can lead to heat waves in certain areas.

在夏季，反气旋发散可能导致某些地区出现热浪。

4.Understanding anticyclone divergence 反气旋发散 is crucial for predicting drought conditions.

理解反气旋发散对于预测干旱条件至关重要。

5.Meteorologists often analyze anticyclone divergence 反气旋发散 patterns to predict changes in weather systems.

气象学家经常分析反气旋发散模式，以预测天气系统的变化。

作文

In the study of meteorology, understanding various atmospheric phenomena is crucial for predicting weather patterns and comprehending climate dynamics. One such phenomenon is the concept of anticyclone divergence, which plays a significant role in shaping weather systems. An anticyclone refers to a high-pressure system characterized by descending air that leads to clear skies and stable weather conditions. When we discuss anticyclone divergence, we are referring to the outward flow of air from the center of this high-pressure system. This process has important implications for weather behavior and environmental conditions.Anticyclones are typically associated with fair weather, as the descending air inhibits cloud formation and precipitation. However, the divergence of air at the surface can lead to interesting effects in the atmosphere. As air diverges from the center of the anticyclone, it creates a region of low pressure at the surface, which can influence nearby weather systems. This divergence can also enhance the stability of the anticyclone itself, reinforcing the clear and calm conditions that are characteristic of these high-pressure systems.Understanding anticyclone divergence is essential for meteorologists when forecasting weather. For instance, when an anticyclone is dominant in a region, the divergence of air can lead to the development of subsidence inversions, where warm air traps cooler air near the surface. This phenomenon can result in prolonged periods of stagnant air, leading to air quality issues and fog formation.Moreover, anticyclone divergence can interact with other weather systems. For example, when an anticyclone is positioned near a low-pressure system, the divergent flow of air can influence the movement and intensity of the low-pressure area. Meteorologists must consider these interactions to provide accurate forecasts, especially in regions prone to rapidly changing weather conditions.The effects of anticyclone divergence are not limited to local weather patterns; they can also have broader climatic implications. For instance, persistent anticyclonic conditions can lead to droughts in certain areas, as the lack of precipitation can severely impact agriculture and water supply. Understanding the mechanisms behind anticyclone divergence allows scientists to better predict these long-term climatic trends and their potential impacts on ecosystems and human activities.In conclusion, anticyclone divergence is a vital concept in meteorology that illustrates the complex interactions within the atmosphere. By studying how air flows outwards from high-pressure systems, meteorologists can gain insights into weather patterns, improve forecasting accuracy, and understand the broader implications for climate. As our understanding of these atmospheric phenomena continues to evolve, the importance of concepts like anticyclone divergence will only grow, highlighting the intricate balance of forces that govern our weather and climate.Through this exploration of anticyclone divergence, we can appreciate the delicate interplay between high-pressure systems and weather behavior, emphasizing the need for ongoing research in the field of meteorology.

在气象学研究中，理解各种大气现象对于预测天气模式和理解气候动态至关重要。其中一个现象是反气旋辐散的概念，它在塑造天气系统方面发挥着重要作用。反气旋是指一种高压系统，其特征是下降的空气导致晴朗的天空和稳定的天气条件。当我们讨论反气旋辐散时，我们指的是来自该高压系统中心的空气向外流动。这一过程对天气行为和环境条件具有重要影响。反气旋通常与良好的天气相关，因为下降的空气抑制了云的形成和降水。然而，表面空气的辐散可能会在大气中产生有趣的效果。随着空气从反气旋中心辐散，它在地面上形成一个低压区，这可能会影响附近的天气系统。这种辐散也可以增强反气旋本身的稳定性，加强这些高压系统特有的晴朗和宁静的条件。理解反气旋辐散对气象学家在天气预报时至关重要。例如，当反气旋在某个区域占主导地位时，空气的辐散可能导致沉降逆温的形成，即温暖的空气将较冷的空气困在近地面。这种现象可能导致长时间的静止空气，造成空气质量问题和雾霭的形成。此外，反气旋辐散还可以与其他天气系统相互作用。例如，当反气旋靠近低压系统时，空气的辐散流动可能会影响低压区的移动和强度。气象学家必须考虑这些相互作用，以提供准确的天气预报，特别是在天气变化迅速的地区。反气旋辐散的影响不仅限于局部天气模式；它们还可能对更广泛的气候产生影响。例如，持续的反气旋条件可能导致某些地区的干旱，因为缺乏降水可能严重影响农业和水供应。理解反气旋辐散背后的机制使科学家能够更好地预测这些长期气候趋势及其对生态系统和人类活动的潜在影响。总之，反气旋辐散是气象学中的一个重要概念，说明了大气中复杂的相互作用。通过研究空气如何从高压系统向外流动，气象学家可以深入了解天气模式，提高预报准确性，并理解对气候的更广泛影响。随着我们对这些大气现象理解的不断发展，像反气旋辐散这样的概念的重要性只会增加，突显出支配我们天气和气候的力量之间微妙的平衡。通过对反气旋辐散的探索，我们可以欣赏到高压系统与天气行为之间的微妙互动，强调了在气象学领域持续研究的必要性。