thermic anti-cyclone

简明释义

热反气旋

英英释义

例句

1.During summer, the thermic anti-cyclone can lead to prolonged heatwaves.

在夏季，热气旋可能导致持续的热浪。

2.The thermic anti-cyclone is responsible for the clear skies and calm weather we are experiencing today.

今天我们所经历的晴朗天空和宁静天气是由热气旋造成的。

3.Meteorologists use satellite imagery to track the development of a thermic anti-cyclone.

气象学家利用卫星图像追踪热气旋的发展。

4.The weather forecast predicts a stable atmosphere due to the presence of a thermic anti-cyclone.

天气预报预测由于存在一个热气旋，大气将保持稳定。

5.Farmers are optimistic about the sunny days ahead, thanks to the thermic anti-cyclone forming over the region.

农民们对即将到来的阳光明媚的日子感到乐观，这要归功于在该地区形成的热气旋。

作文

The atmosphere is a complex system, and understanding its various phenomena is essential for meteorologists and climate scientists. One such phenomenon is the thermic anti-cyclone, which plays a significant role in weather patterns and climatic conditions. A thermic anti-cyclone (热力反气旋) is characterized by a high-pressure system that forms due to temperature differences within the atmosphere. Unlike typical anti-cyclones that are primarily driven by large-scale atmospheric dynamics, thermic anti-cyclones are influenced significantly by local heating effects, such as those caused by sunlight warming the Earth's surface.In regions where the sun's rays are most intense, the ground heats up quickly, causing the air above it to warm as well. As this air warms, it becomes less dense and begins to rise. This upward movement of warm air creates a low-pressure area at the surface. Surrounding cooler air then rushes in to fill this void, leading to the formation of a high-pressure system, or a thermic anti-cyclone (热力反气旋). This process can often be observed in desert areas or during summer months when the temperature variations between day and night are most pronounced.The presence of a thermic anti-cyclone can have several impacts on local weather. For instance, these systems are often associated with clear skies and stable weather conditions. The descending air in a thermic anti-cyclone suppresses cloud formation, leading to sunny days. However, this stability can also result in extreme heat, especially in regions that experience prolonged periods of high pressure. The lack of cloud cover allows for more solar radiation to reach the ground, contributing to rising temperatures.Moreover, thermic anti-cyclones can influence broader climatic conditions. When these systems persist for extended periods, they can lead to droughts, particularly in agricultural regions. The absence of precipitation and the intense heat can stress crops and water supplies, leading to significant economic implications. Conversely, when a thermic anti-cyclone breaks down, it can lead to sudden changes in weather patterns, including thunderstorms or heavy rainfall, as the accumulated moisture in the atmosphere is released.Understanding the dynamics of thermic anti-cyclones is crucial not only for weather forecasting but also for climate modeling. As global temperatures continue to rise due to climate change, the behavior of these systems may also change, leading to more frequent or intense occurrences. Researchers are actively studying how shifts in temperature gradients could alter the frequency and intensity of thermic anti-cyclones and their subsequent impact on local and regional climates.In conclusion, the thermic anti-cyclone (热力反气旋) is a fascinating meteorological phenomenon that illustrates the intricate relationship between temperature and atmospheric pressure. By studying these systems, scientists can gain valuable insights into weather patterns, climate variability, and the potential impacts of climate change. As we continue to explore the complexities of our atmosphere, understanding phenomena like the thermic anti-cyclone will be essential for predicting future weather events and preparing for their consequences.

大气是一个复杂的系统，理解其各种现象对气象学家和气候科学家至关重要。其中一种现象是热力反气旋，它在天气模式和气候条件中发挥着重要作用。热力反气旋（thermic anti-cyclone）以高压系统为特征，形成是由于大气中的温度差异。与主要由大规模大气动力学驱动的典型反气旋不同，热力反气旋受到局部加热效应的显著影响，例如阳光加热地球表面所造成的。在阳光辐射最强的地区，地面迅速升温，导致其上方的空气也变暖。随着空气变暖，它的密度降低，开始上升。这种温暖空气的上升运动在地面上形成了低压区。周围较冷的空气则急忙涌入填补这一空缺，从而导致高压系统的形成，即热力反气旋（thermic anti-cyclone）。这种过程通常可以在沙漠地区或夏季月份观察到，当时昼夜之间的温度变化最为明显。热力反气旋的存在对当地天气有几个影响。例如，这些系统通常与晴朗的天空和稳定的天气条件相关联。热力反气旋中的下沉空气抑制了云的形成，导致阳光明媚的日子。然而，这种稳定性也可能导致极端高温，尤其是在经历长时间高压的地区。缺乏云层覆盖使得更多的太阳辐射能够到达地面，从而促成气温上升。此外，热力反气旋还可以影响更广泛的气候条件。当这些系统持续很长时间时，它们可能导致干旱，特别是在农业地区。降水的缺乏和强烈的高温会给作物和水源带来压力，从而导致重大的经济影响。相反，当热力反气旋崩溃时，可能会导致天气模式的突然变化，包括雷暴或强降雨，因为积聚在大气中的水分被释放出来。理解热力反气旋的动态不仅对于天气预报至关重要，而且对于气候建模也同样重要。随着全球气温因气候变化而持续上升，这些系统的行为也可能发生变化，导致更频繁或更强烈的出现。研究人员正在积极研究温度梯度的变化如何改变热力反气旋的频率和强度及其对地方和区域气候的后续影响。总之，热力反气旋（thermic anti-cyclone）是一个引人入胜的气象现象，展示了温度与大气压力之间错综复杂的关系。通过研究这些系统，科学家可以获得关于天气模式、气候变异性及气候变化潜在影响的宝贵见解。随着我们继续探索大气的复杂性，理解像热力反气旋这样的现象将对预测未来的天气事件及其后果至关重要。