maritime air mass
简明释义
海洋气团
英英释义
A maritime air mass is a large body of air that originates over oceans or large bodies of water, characterized by high humidity and relatively mild temperatures. | 海洋气团是指源自海洋或大型水体的大气团,具有高湿度和相对温和的温度特征。 |
例句
1.Meteorologists are tracking a large maritime air mass (海洋气团) that could lead to heavy rainfall this weekend.
气象学家正在跟踪一个大型的maritime air mass (海洋气团),这可能会导致这个周末的大雨。
2.The maritime air mass (海洋气团) originating from the Pacific Ocean is known for its humidity.
来自太平洋的maritime air mass (海洋气团) 以其湿度而闻名。
3.The transition from a continental to a maritime air mass (海洋气团) often results in a drastic change in weather patterns.
从大陆气团到maritime air mass (海洋气团) 的过渡通常会导致天气模式的剧烈变化。
4.The forecast predicts that a warm maritime air mass (海洋气团) will move into the region, bringing higher temperatures.
天气预报预测,一个温暖的maritime air mass (海洋气团) 将进入该地区,带来更高的气温。
5.As the maritime air mass (海洋气团) interacts with the colder land air, we can expect foggy conditions tomorrow.
由于maritime air mass (海洋气团) 与较冷的陆地空气相互作用,我们可以期待明天出现雾霾天气。
作文
Understanding the concept of a maritime air mass is crucial for grasping the dynamics of weather systems. A maritime air mass refers to a large body of air that originates over oceans or large lakes, characterized by its high humidity and relatively stable temperature. These air masses play a significant role in influencing local and regional climates, particularly in coastal areas. When warm, moist air from a maritime air mass moves over land, it can lead to various weather phenomena, including rain, fog, and even thunderstorms. The formation of a maritime air mass typically occurs when air remains stationary over a body of water for an extended period, allowing it to absorb moisture and adjust to the temperature of the water below. This process is essential for the development of weather patterns, as the interaction between maritime air masses and continental air masses can result in significant meteorological events. For instance, when a maritime air mass meets a cold, dry air mass from land, it can create instability in the atmosphere, leading to precipitation and storms.In addition to their impact on precipitation, maritime air masses also influence temperature variations along coastlines. Coastal regions often experience milder temperatures compared to inland areas due to the moderating effect of the ocean. The presence of a maritime air mass can prevent extreme temperature fluctuations, resulting in a more temperate climate. This is particularly evident in places like San Francisco, where the cool, moist air from the Pacific Ocean helps maintain a moderate climate year-round.Moreover, the movement of maritime air masses can have broader implications for global weather patterns. For example, during the summer months, warm maritime air masses can travel northward, bringing increased humidity and heat to regions that are typically cooler. Conversely, in winter, the same air masses can contribute to milder conditions in areas that would otherwise experience harsh cold spells. Understanding these patterns is vital for meteorologists and climate scientists as they work to predict weather changes and prepare for potential natural disasters.In conclusion, the significance of maritime air masses in weather systems cannot be overstated. Their ability to transport moisture and moderate temperatures makes them a key component in the study of meteorology. As climate change continues to affect global weather patterns, understanding the behavior and characteristics of maritime air masses will become increasingly important. By studying these air masses, scientists can better predict weather events and help communities prepare for the impacts of changing climate conditions. Overall, a comprehensive understanding of maritime air masses enhances our knowledge of the complex interactions between the atmosphere and the Earth's surface, ultimately contributing to more effective weather forecasting and climate resilience strategies.
理解“海洋气团”这一概念对于掌握天气系统的动态至关重要。海洋气团是指起源于海洋或大湖的大面积空气体,具有高湿度和相对稳定的温度。这些气团在影响局部和区域气候方面发挥着重要作用,特别是在沿海地区。当来自海洋气团的温暖潮湿空气移动到陆地上时,会导致各种天气现象,包括降雨、雾霭甚至雷暴。海洋气团的形成通常发生在空气在水体上方停留一段时间后,使其能够吸收水分并适应水下的温度。这一过程对于天气模式的发展至关重要,因为海洋气团与大陆气团之间的相互作用可以导致显著的气象事件。例如,当一个海洋气团遇到来自陆地的寒冷干燥气团时,会在大气中产生不稳定性,导致降水和风暴。除了对降水的影响外,海洋气团还影响沿海地区的温度变化。由于海洋的调节作用,沿海地区的温度通常比内陆地区更温和。海洋气团的存在可以防止极端温度波动,从而导致更温和的气候。这在旧金山等地尤为明显,太平洋的凉爽潮湿空气帮助维持了全年温和的气候。此外,海洋气团的移动可能对全球天气模式产生更广泛的影响。例如,在夏季,温暖的海洋气团可以向北移动,为通常较凉的地区带来更多的湿气和热量。反之,在冬季,同样的气团可以使本会经历严寒的地区出现较温和的条件。了解这些模式对于气象学家和气候科学家至关重要,因为他们致力于预测天气变化并为潜在的自然灾害做好准备。总之,海洋气团在天气系统中的重要性不容小觑。它们传输湿气和调节温度的能力使它们成为气象研究的关键组成部分。随着气候变化继续影响全球天气模式,理解海洋气团的行为和特征将变得越来越重要。通过研究这些气团,科学家可以更好地预测天气事件,并帮助社区为气候条件变化的影响做好准备。总体而言,对海洋气团的全面理解增强了我们对大气与地球表面之间复杂相互作用的认识,从而有助于更有效的天气预报和气候韧性策略。
相关单词