Okhotsk high

简明释义

鄂霍次克海高压

英英释义

例句

1.The stability provided by the Okhotsk high (鄂霍次克高压) helps in reducing storm activity in the area.

由Okhotsk high (鄂霍次克高压) 提供的稳定性有助于减少该地区的风暴活动。

2.Meteorologists are tracking the movement of the Okhotsk high (鄂霍次克高压) as it shifts towards the Japanese archipelago.

气象学家正在跟踪Okhotsk high (鄂霍次克高压) 的移动，因为它正向日本群岛移动。

3.During summer, the influence of the Okhotsk high (鄂霍次克高压) can lead to cooler temperatures in northern Japan.

夏季时，Okhotsk high (鄂霍次克高压) 的影响可能导致日本北部气温降低。

4.The weather forecast indicates that the Okhotsk high (鄂霍次克高压) will dominate the region this week, bringing clear skies.

天气预报显示本周将有Okhotsk high (鄂霍次克高压) 主导该地区，带来晴朗的天空。

5.Farmers rely on the presence of the Okhotsk high (鄂霍次克高压) for favorable growing conditions.

农民依赖Okhotsk high (鄂霍次克高压) 的存在以获得良好的生长条件。

作文

The term Okhotsk high refers to a significant atmospheric pressure system that forms over the Sea of Okhotsk, located in the northwestern Pacific Ocean. This high-pressure area is characterized by stable weather conditions and plays a crucial role in influencing the climate of the surrounding regions, including parts of Russia and Japan. Understanding the dynamics of the Okhotsk high is essential for meteorologists and climatologists as it affects not only local weather patterns but also broader climatic phenomena such as the East Asian monsoon. The formation of the Okhotsk high typically occurs during the summer months when the land heats up more quickly than the sea. This temperature difference leads to the development of high pressure over the cooler waters of the Sea of Okhotsk. As a result, the air over this region becomes denser and sinks, creating a stable atmosphere that prevents cloud formation and precipitation. Consequently, areas influenced by the Okhotsk high often experience clear skies and warm temperatures during this time. Conversely, during the winter months, the situation changes dramatically. The Okhotsk high tends to strengthen due to the cooling of the land and the sea. The cold air masses that develop over the Sea of Okhotsk can lead to harsh winter conditions in nearby regions, including heavy snowfall and frigid temperatures. This seasonal variability highlights the importance of the Okhotsk high in shaping the climatic conditions of northeastern Asia. In addition to its direct effects on weather, the Okhotsk high is also linked to larger scale atmospheric patterns. For example, it can influence the strength and position of the jet stream, which in turn affects weather systems across the entire Northern Hemisphere. The interaction between the Okhotsk high and other pressure systems can lead to significant weather events, such as typhoons and heavy rainfalls, particularly in Japan and the Korean Peninsula. Furthermore, the study of the Okhotsk high has implications for understanding climate change. As global temperatures rise, the behavior of this high-pressure system may alter, potentially leading to changes in regional climates. Researchers are keenly observing these trends to predict future weather patterns and their impacts on agriculture, water resources, and ecosystems in the affected areas. In conclusion, the Okhotsk high is a vital component of the atmospheric system in northeastern Asia. Its influence extends beyond mere weather conditions, affecting climate, agriculture, and even the daily lives of millions of people. By studying the Okhotsk high, scientists can gain valuable insights into the complexities of our planet's climate system and better prepare for the challenges posed by climate variability and change.

术语Okhotsk high指的是一个重要的大气压力系统，它形成于位于西北太平洋的鄂霍次克海上。这个高压区域以稳定的天气条件为特征，并在影响周边地区（包括俄罗斯和日本部分地区）的气候方面发挥着关键作用。理解Okhotsk high的动态对于气象学家和气候学家至关重要，因为它不仅影响当地的天气模式，还影响更广泛的气候现象，如东亚季风。Okhotsk high的形成通常发生在夏季，当陆地的温度升高速度快于海洋时。这种温差导致在较冷的鄂霍次克海水域上形成高压。结果，该区域的空气变得更加密集并下沉，形成了一个稳定的大气，阻止了云的形成和降水。因此，受Okhotsk high影响的地区在此期间往往经历晴朗的天空和温暖的气温。相反，在冬季，情况会发生剧烈变化。由于陆地和海洋的降温，Okhotsk high往往会增强。在鄂霍次克海上形成的寒冷气团可能导致附近地区出现严酷的冬季条件，包括大雪和严寒气温。这种季节性变化突显了Okhotsk high在塑造东北亚气候条件中的重要性。除了对天气的直接影响外，Okhotsk high还与更大规模的大气模式相关。例如，它可以影响喷流的强度和位置，从而影响整个北半球的天气系统。Okhotsk high与其他压力系统之间的相互作用可能导致显著的天气事件，例如台风和强降雨，特别是在日本和朝鲜半岛。此外，研究Okhotsk high对理解气候变化也具有重要意义。随着全球气温上升，这个高压系统的行为可能会改变，可能导致区域气候的变化。研究人员正在密切观察这些趋势，以预测未来的天气模式及其对农业、水资源和生态系统的影响。总之，Okhotsk high是东北亚大气系统的重要组成部分。它的影响超出了单纯的天气条件，影响着气候、农业，甚至数百万人的日常生活。通过研究Okhotsk high，科学家们可以深入了解我们星球气候系统的复杂性，并更好地为气候变异和变化带来的挑战做好准备。