thermal wind

简明释义

热成风

英英释义

例句

1.In coastal areas, thermal wind 热风 can influence the local climate significantly.

在沿海地区，热风可以显著影响当地气候。

2.During the summer, the thermal wind 热风 effect can lead to increased temperatures in urban areas.

夏季，热风效应可能导致城市地区气温升高。

3.The interaction between land and sea creates a specific thermal wind 热风 pattern that affects fishing conditions.

陆地与海洋之间的相互作用创造了特定的热风模式，影响渔业条件。

4.Meteorologists use thermal wind 热风 calculations to predict storm movements more accurately.

气象学家使用热风计算来更准确地预测风暴的移动。

5.The concept of thermal wind 热风 is crucial for understanding weather patterns in mountainous regions.

热风的概念对于理解山区的天气模式至关重要。

作文

The concept of thermal wind refers to the wind patterns that are primarily caused by temperature differences in the atmosphere. This phenomenon is crucial for understanding various weather systems and their behaviors. When the sun heats the Earth's surface, it creates areas of warm air that rise, leading to a drop in pressure. Surrounding cooler air then rushes in to fill this void, resulting in winds. The thermal wind plays a significant role in the development of local and regional climates, influencing everything from sea breezes to mountain winds.In meteorology, the thermal wind is often analyzed in conjunction with the concept of geostrophic balance, which describes the relationship between the pressure gradient force and the Coriolis effect. As air moves from high-pressure areas to low-pressure areas, the rotation of the Earth causes the wind to curve, creating a balance that is essential for predicting weather patterns. The thermal wind can also be observed in larger scale phenomena, such as cyclones and anticyclones, where the temperature gradients between different air masses can lead to significant wind patterns.One of the most common examples of thermal wind can be seen in coastal areas. During the day, land heats up faster than the ocean, causing the air above the land to become warmer and rise. This action creates a low-pressure area over the land, prompting cooler air from the ocean to move in, resulting in a sea breeze. Conversely, at night, the land cools more quickly than the ocean, leading to an offshore breeze as the warmer air over the ocean rises. This daily cycle of thermal wind is a perfect illustration of how temperature differences drive wind patterns.In mountainous regions, thermal wind can create unique weather conditions. As the sun heats the slopes during the day, warm air rises and creates an updraft, known as a valley breeze. At night, the cooling air descends, resulting in a down-slope wind called a katabatic wind. These winds can significantly affect local weather and even influence the ecosystems found in these areas.Understanding thermal wind is not only important for meteorologists but also for various industries such as aviation, agriculture, and renewable energy. For instance, pilots must consider thermal wind when planning flight paths, as it can impact aircraft performance. Farmers may also need to account for thermal wind when deciding on the best times to plant or harvest crops, as winds can affect moisture levels and temperature.In conclusion, the study of thermal wind is essential for comprehending the complex interactions between temperature and atmospheric movement. By recognizing how temperature differences generate wind patterns, we can better predict weather changes and understand their implications for our daily lives. As climate change continues to alter weather patterns globally, the significance of thermal wind will only become more pronounced, making it a vital area of research for future meteorologists and climate scientists.

“热风”这一概念指的是主要由大气中的温度差异引起的风模式。这一现象对于理解各种天气系统及其行为至关重要。当太阳加热地球表面时，会产生温暖的空气区，这些空气上升，导致气压下降。周围较冷的空气随后迅速涌入以填补这一空缺，从而形成风。“热风”在地方和区域气候的发展中扮演着重要角色，影响着从海风到山风的一切。在气象学中，“热风”通常与地转平衡的概念一起分析，后者描述了压力梯度力与科里奥利效应之间的关系。当空气从高压区移动到低压区时，地球的自转使得风发生曲折，形成一种平衡，这对于预测天气模式至关重要。“热风”也可以在更大规模的现象中观察到，例如气旋和反气旋，其中不同气团之间的温度梯度可以导致显著的风模式。“热风”的一个常见例子可以在沿海地区看到。白天，陆地加热速度快于海洋，导致陆地上方的空气变得更温暖并上升。这一过程在陆地上形成一个低压区，促使来自海洋的凉爽空气移动进来，形成海风。相反，在夜间，陆地冷却速度快于海洋，导致离岸风的形成，因为海洋上方的温暖空气上升。这种“热风”的日常循环完美地说明了温度差异如何驱动风模式。在山区，“热风”可以创造出独特的天气条件。白天，阳光加热山坡，温暖的空气上升，形成上升气流，被称为山谷微风。夜间，冷却的空气下降，形成下坡风，称为下坡风。这些风可以显著影响当地天气，甚至影响这些地区的生态系统。理解“热风”不仅对气象学家重要，对航空、农业和可再生能源等各个行业也至关重要。例如，飞行员在规划航线时必须考虑“热风”，因为它会影响飞机的性能。农民在决定最佳的播种或收获时间时，也可能需要考虑“热风”，因为风会影响湿度水平和温度。总之，研究“热风”对于理解温度与大气运动之间复杂的相互作用至关重要。通过认识到温度差异如何产生风模式，我们可以更好地预测天气变化，并理解其对我们日常生活的影响。随着气候变化继续改变全球天气模式，“热风”的重要性将变得更加明显，使其成为未来气象学家和气候科学家研究的重要领域。